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New Horizons
New Horizons space probe
NamesNew Frontiers 1
Mission typePluto/Arrokoth flyby
OperatorNASA
COSPAR ID2006-001A Edit this at Wikidata
SATCAT no.28928Edit this on Wikidata
Websitepluto.jhuapl.edu
science.nasa.gov
Mission durationPrimary: 9.5 years
Elapsed: 19 years, 9 months, 9 days
Spacecraft properties
ManufacturerAPL / SwRI
Launch mass478 kg (1,054 lb)[1]
Dry mass401 kg (884 lb)
Payload mass30.4 kg (67 lb)
Dimensions2.2 × 2.1 × 2.7 m (7.2 × 6.9 × 8.9 ft)
Power245 watts
Start of mission
Launch dateJanuary 19, 2006, 19:00:00.221 (2006-01-19UTC19) UTC (2:00 pm EST)[2]
RocketAtlas V (551) AV-010[2]
Launch siteCape Canaveral, SLC‑41
ContractorInternational Launch Services[3]
Orbital parameters
Eccentricity1.41905
Inclination2.23014°
EpochJanuary 1, 2017 (JD 2457754.5)[4]
Flyby of 132524 APL (incidental)
Closest approachJune 13, 2006, 04:05 UTC
Distance101,867 km (63,297 mi)
Flyby of Jupiter (gravity assist)
Closest approachFebruary 28, 2007, 05:43:40 UTC
Distance2,300,000 km (1,400,000 mi)
Flyby of Pluto
Closest approachJuly 14, 2015, 11:49:57 UTC
Distance12,500 km (7,800 mi)
Flyby of Charon (moon)
Closest approachJuly 14, 2015, 12:02:22 UTC
Distance29,431 km (18,288 mi)
Flyby of 486958 Arrokoth
Closest approachJanuary 1, 2019, 05:33:00 UTC
Distance3,500 km (2,200 mi)
Juno →
New Horizons before launch

New Horizons is an interplanetary space probe launched as a part of NASA's New Frontiers program.[5] It was launched in 2006, becoming the first spacecraft to perform a flyby study of the Pluto system in 2015. A secondary mission contained a flyby and study of one or more other Kuiper belt objects (KBOs) in the decade to follow, where it flew past 486958 Arrokoth in 2019.

It was engineered by the Johns Hopkins University Applied Physics Laboratory (APL) and the Southwest Research Institute (SwRI), with a team led by Alan Stern.[6] New Horizons is the fifth space probe to achieve the escape velocity needed to leave the Solar System.

On January 19, 2006, New Horizons was launched from Cape Canaveral Space Force Station by an Atlas V rocket directly into an Earth-and-solar escape trajectory with a speed of about 16.26 km/s (10.10 mi/s; 58,500 km/h; 36,400 mph). It was the fastest (average speed with respect to Earth) human-made object ever launched from Earth.[7][8][9][10] It is not the fastest speed recorded for a spacecraft, which, as of 2023, is that of the Parker Solar Probe. After a brief encounter with asteroid 132524 APL, New Horizons proceeded to Jupiter, making its closest approach on February 28, 2007, at a distance of 2.3 million kilometers (1.4 million miles). The Jupiter flyby provided a gravity assist that increased New Horizons' speed; the flyby also enabled a general test of New Horizons' scientific capabilities, returning data about the planet's atmosphere, moons, and magnetosphere.

Most of the post-Jupiter voyage was spent in hibernation mode to preserve onboard systems, except for brief annual checkouts.[11] On December 6, 2014, New Horizons was brought back online for the Pluto encounter, and instrument check-out began.[12] On January 15, 2015, the spacecraft began its approach phase to Pluto.

On July 14, 2015, at 11:49 UTC, it flew 12,500 km (7,800 mi) above the surface of Pluto,[13][14] which at the time was 34 AU from the Sun,[15] making it the first spacecraft to explore the dwarf planet.[16] In August 2016, New Horizons was reported to have traveled at speeds of more than 84,000 km/h (52,000 mph).[17] On October 25, 2016, at 21:48 UTC, the last recorded data from the Pluto flyby was received from New Horizons.[18] Having completed its flyby of Pluto,[19] New Horizons then maneuvered for a flyby of Kuiper belt object 486958 Arrokoth (then nicknamed Ultima Thule),[20][21][22] which occurred on January 1, 2019,[23][24] when it was 43.4 AU (6.49 billion km; 4.03 billion mi) from the Sun.[20][21] In August 2018, NASA cited results by Alice on New Horizons to confirm the existence of a "hydrogen wall" at the outer edges of the Solar System. This "wall" was first detected in 1992 by the two Voyager spacecraft.[25][26]

New Horizons is traveling through the Kuiper belt; it is 62.23 AU (9.31 billion km; 5.78 billion mi) from Earth and 62.71 AU (9.38 billion km; 5.83 billion mi) from the Sun as of September 2025.[27] NASA has announced it is to extend operations for New Horizons until the spacecraft exits the Kuiper belt, which is expected to occur in either 2028 or 2029,[28] but the proposed budget for FY2026 cuts funding for New Horizons, and it is set for shut down.[29]

History

[edit]
Early concept art of the New Horizons spacecraft. The mission, led by the Applied Physics Laboratory and Alan Stern, eventually became the first mission to Pluto.

In August 1992, JPL scientist Robert Staehle called Pluto discoverer Clyde Tombaugh, requesting permission to visit his planet. "I told him he was welcome to it," Tombaugh later remembered, "though he's got to go one long, cold trip."[30] The call eventually led to a series of proposed Pluto missions leading up to New Horizons.

Stamatios "Tom" Krimigis, head of the Applied Physics Laboratory's space division, one of many entrants in the New Frontiers Program competition, formed the New Horizons team with Alan Stern in December 2000. Appointed as the project's principal investigator, Stern was described by Krimigis as "the personification of the Pluto mission".[31] New Horizons was based largely on Stern's work since Pluto 350 and involved most of the team from Pluto Kuiper Express.[32]

The New Horizons proposal was one of five that were officially submitted to NASA. It was later selected as one of two finalists to be subject to a three-month concept study in June 2001. The other finalist, POSSE (Pluto and Outer Solar System Explorer), was a separate but similar Pluto mission concept by the University of Colorado Boulder, led by principal investigator Larry W. Esposito, and supported by the JPL, Lockheed Martin and the University of California.[33]

However, the APL, in addition to being supported by Pluto Kuiper Express developers at the Goddard Space Flight Center and Stanford University[33] were at an advantage; they had recently developed NEAR Shoemaker for NASA, which had successfully entered orbit around 433 Eros earlier that year, and would later land on the asteroid to scientific and engineering fanfare.[34]

In November 2001, New Horizons was officially selected for funding as part of the New Frontiers program.[35] However, the new NASA Administrator appointed by the Bush administration, Sean O'Keefe, was not supportive of New Horizons and effectively canceled it by not including it in NASA's budget for 2003. NASA's Associate Administrator for the Science Mission Directorate, Ed Weiler, prompted Stern to lobby for the funding of New Horizons in hopes of the mission appearing in the Planetary Science Decadal Survey, a prioritized "wish list", compiled by the United States National Research Council, that reflects the opinions of the scientific community.[31]

After an intense campaign to gain support for New Horizons, the Planetary Science Decadal Survey of 2003–2013 was published in the summer of 2002. New Horizons topped the list of projects considered the highest priority among the scientific community in the medium-size category; ahead of missions to the Moon, and even Jupiter. Weiler stated that it was a result that "[his] administration was not going to fight".[31] Funding for the mission was finally secured following the publication of the report. Stern's team was finally able to start building the spacecraft and its instruments, with a planned launch in January 2006 and arrival at Pluto in 2015.[31] Alice Bowman became Mission Operations Manager (MOM).[36]

Mission profile

[edit]
An artist's impression of New Horizons' close encounter with the Plutonian system

New Horizons is the first mission in NASA's New Frontiers mission category, larger and more expensive than the Discovery missions but smaller than the missions of the Flagship Program. The cost of the mission, including spacecraft and instrument development, launch vehicle, mission operations, data analysis, and education/public outreach, is approximately $700 million over 15 years (2001–2016).[37] The spacecraft was built primarily by Southwest Research Institute (SwRI) and the Johns Hopkins Applied Physics Laboratory. The mission's principal investigator is Alan Stern of the Southwest Research Institute (formerly NASA Associate Administrator).

After separation from the launch vehicle, overall control was taken by Mission Operations Center (MOC) at the Applied Physics Laboratory in Howard County, Maryland. The science instruments are operated at Clyde Tombaugh Science Operations Center (T-SOC) in Boulder, Colorado.[38] Navigation is performed at various contractor facilities, whereas the navigational positional data and related celestial reference frames are provided by the Naval Observatory Flagstaff Station through Headquarters NASA and JPL.

KinetX is the lead on the New Horizons navigation team and is responsible for planning trajectory adjustments as the spacecraft speeds toward the outer Solar System. Coincidentally the Naval Observatory Flagstaff Station was where the photographic plates were taken for the discovery of Pluto's moon Charon. The Naval Observatory itself is not far from the Lowell Observatory where Pluto was discovered.

New Horizons was originally planned as a voyage to the only unexplored planet in the Solar System. When the spacecraft was launched, Pluto was still classified as a planet, later to be reclassified as a dwarf planet by the International Astronomical Union (IAU). Some members of the New Horizons team, including Alan Stern, disagree with the IAU definition and still describe Pluto as the ninth planet.[39] Pluto's satellites Nix and Hydra also have a connection with the spacecraft: the first letters of their names (N and H) are the initials of New Horizons. The moons' discoverers chose these names for this reason, plus Nix and Hydra's relationship to the mythological Pluto.[40]

Mementos

[edit]

In addition to the science equipment, there are nine cultural artifacts traveling with the spacecraft.[41] These include a collection of 434,738 names stored on a compact disc,[42][43] a collection of images of New Horizons project personnel on another CD, a piece of Scaled Composites's SpaceShipOne,[44] a "Not Yet Explored" USPS stamp,[45][46] and two copies of the Flag of the United States.[47][41]

About 30 grams (1 oz) of 'Clyde Tombaugh's ashes are aboard the spacecraft, to commemorate his discovery of Pluto in 1930.[48][49] A Florida state quarter coin, whose design commemorates human exploration, is included, officially as a trim weight,[50] as is a Maryland state quarter to honor the probe's builders.[41] One of the science packages (a dust counter) is named after Venetia Burney, who, as a child, suggested the name "Pluto" after its discovery.

Goal

[edit]
View of Mission Operations at the Applied Physics Laboratory in Laurel, Maryland (July 14, 2015)

The goal of the mission is to understand the formation of the Plutonian system, the Kuiper belt, and the transformation of the early Solar System.[51] The spacecraft collected data on the atmospheres, surfaces, interiors, and environments of Pluto and its moons. It will also study other objects in the Kuiper belt.[52] "By way of comparison, New Horizons gathered 5,000 times as much data at Pluto as Mariner did at the Red Planet."[53]

Some of the questions the mission attempts to answer are: What is Pluto's atmosphere made of and how does it behave? What does its surface look like? Are there large geological structures? How do solar wind particles interact with Pluto's atmosphere?[54]

Specifically, the mission's science objectives are to:[55]

  • Map the surface compositions of Pluto and Charon
  • Characterize the geologies and morphologies of Pluto and Charon
  • Characterize the neutral atmosphere of Pluto and its escape rate
  • Search for an atmosphere around Charon
  • Map surface temperatures on Pluto and Charon
  • Search for rings and additional satellites around Pluto
  • Conduct similar investigations of one or more Kuiper belt objects

Design and construction

[edit]
Interactive 3D model of New Horizons
An interactive 3D model of New Horizons

Spacecraft subsystems

[edit]
New Horizons in a clean room at Kennedy Space Center in 2005

The spacecraft is comparable in size and general shape to a grand piano and has been compared to a piano glued to a cocktail bar-sized satellite dish.[56] As a point of departure, the team took inspiration from the Ulysses spacecraft,[57] which also carried a radioisotope thermoelectric generator (RTG) and dish on a box-in-box structure through the outer Solar System. Many subsystems and components have flight heritage from APL's CONTOUR spacecraft, which in turn had heritage from APL's TIMED spacecraft.

New Horizons' body forms a triangle, almost 0.76 m (2.5 ft) thick. (The Pioneers have hexagonal bodies, whereas the Voyagers have decagonal bodies,[58] Galileo an octagonal prism body,[59] and Cassini–Huygens a dodecagonal prism body.[60]) A 7075 aluminium alloy tube forms the main structural column, between the launch vehicle adapter ring at the "rear", and the 2.1 m (6 ft 11 in) radio dish antenna affixed to the "front" flat side. The titanium fuel tank is in this tube. The RTG attaches with a 4-sided titanium mount resembling a gray pyramid or stepstool.

Titanium provides strength and thermal isolation. The rest of the triangle is primarily sandwich panels of thin aluminum face sheet (less than 164 in or 0.40 mm) bonded to aluminum honeycomb core. The structure is larger than strictly necessary, with empty space inside. The structure is designed to act as shielding, reducing electronics errors caused by radiation from the RTG. Also, the mass distribution required for a spinning spacecraft demands a wider triangle.

The interior structure is painted black to equalize temperature by radiative heat transfer. Overall, the spacecraft is thoroughly blanketed to retain heat. Unlike the Pioneers and Voyagers, the radio dish is also enclosed in blankets that extend to the body. The heat from the RTG adds warmth to the spacecraft while it is in the outer Solar System. While in the inner Solar System, the spacecraft must prevent overheating, hence electronic activity is limited, power is diverted to shunts with attached radiators, and louvers are opened to radiate excess heat. While the spacecraft is cruising inactively in the cold outer Solar System, the louvers are closed, and the shunt regulator reroutes power to electric heaters.

Propulsion and attitude control

[edit]

New Horizons has both spin-stabilized (cruise) and three-axis stabilized (science) modes controlled entirely with hydrazine monopropellant. Additional post launch delta-v of over 290 m/s (1,000 km/h; 650 mph) is provided by a 77 kg (170 lb) internal tank. Helium is used as a pressurant, with an elastomeric diaphragm assisting expulsion. The spacecraft's on-orbit mass including fuel is over 470 kg (1,040 lb) on the Jupiter flyby trajectory, but would have been only 445 kg (981 lb) for the backup direct flight option to Pluto. Significantly, had the backup option been taken, this would have meant less fuel for later Kuiper belt operations.

There are 16 thrusters on New Horizons: four 4.4 N (1.0 lbf) and twelve 0.9 N (0.2 lbf) plumbed into redundant branches. The larger thrusters are used primarily for trajectory corrections, and the small ones (previously used on Cassini and the Voyager spacecraft) are used primarily for attitude control and spinup/spindown maneuvers. Two star cameras are used to measure the spacecraft attitude. They are mounted on the face of the spacecraft and provide attitude information while in spin-stabilized or 3-axis mode. In between the time of star camera readings, spacecraft orientation is provided by dual redundant miniature inertial measurement units. Each unit contains three solid-state gyroscopes and three accelerometers. Two Adcole Sun sensors provide attitude determination. One detects the angle to the Sun, whereas the other measures spin rate and clocking.

Power

[edit]
New Horizons' RTG

A cylindrical radioisotope thermoelectric generator (RTG) protrudes in the plane of the triangle from one vertex of the triangle. The RTG provided 245.7 W of power at launch, and was predicted to drop approximately 3.5 W every year, decaying to 202 W by the time of its encounter with the Plutonian system in 2015 and will decay too far to power the transmitters in the 2030s.[6] There are no onboard batteries since RTG output is predictable, and load transients are handled by a capacitor bank and fast circuit breakers. As of January 2019, the power output of the RTG is about 190 W.[61]

The RTG, model "GPHS-RTG", was originally a spare from the Cassini mission. The RTG contains 9.75 kg (21.5 lb) of plutonium-238 oxide pellets.[32] Each pellet is clad in iridium, then encased in a graphite shell. It was developed by the U.S. Department of Energy at the Materials and Fuels Complex, a part of the Idaho National Laboratory.[62] The original RTG design called for 10.9 kg (24 lb) of plutonium, but a unit less powerful than the original design goal was produced because of delays at the United States Department of Energy, including security activities, that delayed plutonium production.[63] The mission parameters and observation sequence had to be modified for the reduced wattage; still, not all instruments can operate simultaneously. The Department of Energy transferred the space battery program from Ohio to Argonne in 2002 because of security concerns.

The amount of radioactive plutonium in the RTG is about one-third the amount on board the Cassini–Huygens probe when it launched in 1997. The Cassini launch had been protested by multiple organizations, due to the risk of such a large amount of plutonium being released into the atmosphere in case of an accident. The United States Department of Energy estimated the chances of a launch accident that would release radiation into the atmosphere at 1 in 350, and monitored the launch[64] because of the inclusion of an RTG on board. It was estimated that a worst-case scenario of total dispersal of on-board plutonium would spread the equivalent radiation of 80% the average annual dosage in North America from background radiation over an area with a radius of 105 km (65 mi).[65]

Flight computer

[edit]

The spacecraft carries two computer systems: the Command and Data Handling system and the Guidance and Control processor. Each of the two systems is duplicated for redundancy, for a total of four computers. The processor used for its flight computers is the Mongoose-V, a 12 MHz radiation-hardened version of the MIPS R3000 CPU. Multiple redundant clocks and timing routines are implemented in hardware and software to help prevent faults and downtime. To conserve heat and mass, spacecraft and instrument electronics are housed together in IEMs (integrated electronics modules). There are two redundant IEMs. Including other functions such as instrument and radio electronics, each IEM contains 9 boards.[66] The software of the probe runs on Nucleus RTOS operating system.[67]

There have been two "safing" events, that sent the spacecraft into safe mode:

  • On March 19, 2007, the Command and Data Handling computer experienced an uncorrectable memory error and rebooted itself, causing the spacecraft to go into safe mode. The craft fully recovered within two days, with some data loss on Jupiter's magnetotail. No impact on the subsequent mission was expected.[68]
  • On July 4, 2015, there was a CPU safing event triggered by an over-assignment of commanded science operations on the craft's approach to Pluto. Fortunately, the craft was able to recover within two days without major impacts on its mission. NASA scientists therefore reduced the number of scientific operations on the craft to prevent future events, which could happen during the approach with Pluto.[69][70]

Telecommunications and data handling

[edit]
New Horizons' antenna, with some test equipment attached.

Communication with the spacecraft is via X band. The craft had a communication rate of 38 kbit/s at Jupiter; at Pluto's distance, a rate of approximately kbit/s per transmitter was expected. Besides the low data rate, Pluto's distance also causes a latency of about 4.5 hours (one-way). The 70 m (230 ft) NASA Deep Space Network (DSN) dishes are used to relay commands once the spacecraft is beyond Jupiter. The spacecraft uses dual modular redundancy transmitters and receivers, and either right- or left-hand circular polarization.

The downlink signal is amplified by dual redundant 12-watt traveling-wave tube amplifiers (TWTAs) mounted on the body under the dish. The receivers are low-power designs. The system can be controlled to power both TWTAs at the same time, and transmit a dual-polarized downlink signal to the DSN that nearly doubles the downlink rate. DSN tests early in the mission with this dual polarization combining technique were successful, and the capability was declared to be operational (when the spacecraft power budget permits both TWTAs to be powered).

In addition to the high-gain antenna, there are two backup low-gain antennas and a medium-gain dish. The high-gain dish has a Cassegrain reflector layout, composite construction, of 2.1-meter (7 ft) diameter providing over 42 dBi of gain and a half-power beam width of about a degree. The prime-focus medium-gain antenna, with a 0.3-meter (1 ft) aperture and 10° half-power beam width, is mounted to the forward-facing side of the high-gain antenna's secondary reflector. The forward low-gain antenna is stacked atop the feed of the medium-gain antenna. The aft low-gain antenna is mounted within the launch adapter at the rear of the spacecraft. This antenna was used only for early mission phases near Earth, just after launch and for emergencies if the spacecraft had lost attitude control.

New Horizons recorded scientific instrument data to its solid-state memory buffer at each encounter, then transmitted the data to Earth. Data storage is done on two low-power solid-state recorders (one primary, one backup) holding up to gigabytes each. Because of the extreme distance from Pluto and the Kuiper belt, only one buffer load at those encounters can be saved. This is because New Horizons would require approximately 16 months after leaving the vicinity of Pluto to transmit the buffer load back to Earth.[71] At Pluto's distance, radio signals from the space probe back to Earth took four hours and 25 minutes to traverse 4.7 billion km of space.[72]

Part of the reason for the delay between the gathering of and transmission of data is that all of the New Horizons instrumentation is body-mounted. In order for the cameras to record data, the entire probe must turn, and the one-degree-wide beam of the high-gain antenna was not pointing toward Earth. Previous spacecraft, such as the Voyager program probes, had a rotatable instrumentation platform (a "scan platform") that could take measurements from virtually any angle without losing radio contact with Earth. New Horizons was mechanically simplified to save weight, shorten the schedule, and improve reliability during its 15-year designed lifetime.

Instruments

[edit]

New Horizons carries seven instruments: three optical instruments, two plasma instruments, a dust sensor and a radio science receiver/radiometer. The instruments are to be used to investigate the global geology, surface composition, surface temperature, atmospheric pressure, atmospheric temperature and escape rate of Pluto and its moons. The rated power is 21 watts, though not all instruments operate simultaneously.[73] In addition, New Horizons has an Ultrastable Oscillator subsystem, which may be used to study and test the Pioneer anomaly towards the end of the spacecraft's life.[74]

Long-Range Reconnaissance Imager (LORRI)

[edit]
LORRI—long-range camera

The Long-Range Reconnaissance Imager (LORRI) is a long-focal-length imager designed for high resolution and responsivity at visible wavelengths. The instrument is equipped with a 1024×1024 pixel by 12-bits-per-pixel monochromatic CCD imager giving a resolution of 5 μrad (~1 arcsec).[75] The CCD is chilled far below freezing by a passive radiator on the antisolar face of the spacecraft. This temperature differential requires insulation and isolation from the rest of the structure. The 208.3 mm (8.20 in) aperture Ritchey–Chretien mirrors and metering structure are made of silicon carbide to boost stiffness, reduce weight and prevent warping at low temperatures. The optical elements sit in a composite light shield and mount with titanium and fiberglass for thermal isolation. Overall mass is 8.6 kg (19 lb), with the optical tube assembly (OTA) weighing about 5.6 kg (12 lb),[76] for one of the largest silicon-carbide telescopes flown at the time (now surpassed by Herschel). For viewing on public web sites the 12-bit per pixel LORRI images are converted to 8-bit per pixel JPEG images.[75] These public images do not contain the full dynamic range of brightness information available from the raw LORRI images files.[75]

Principal investigator: Andy Cheng, Applied Physics Laboratory, Data: LORRI image search at jhuapl.edu[77]

Solar Wind Around Pluto (SWAP)

[edit]
SWAP – Solar Wind Around Pluto

Solar Wind Around Pluto (SWAP) is a toroidal electrostatic analyzer and retarding potential analyzer (RPA), that makes up one of the two instruments comprising New Horizons' Plasma and high-energy particle spectrometer suite (PAM), the other being PEPSSI. SWAP measures particles of up to 6.5 keV and, because of the tenuous solar wind at Pluto's distance, the instrument is designed with the largest aperture of any such instrument ever flown.[78]

Principal investigator: David McComas, Southwest Research Institute

Pluto Energetic Particle Spectrometer Science Investigation (PEPSSI)

[edit]

Pluto Energetic Particle Spectrometer Science Investigation (PEPSSI) is a time of flight ion and electron sensor that makes up one of the two instruments comprising New Horizons' plasma and high-energy particle spectrometer suite (PAM), the other being SWAP. Unlike SWAP, which measures particles of up to 6.5 keV, PEPSSI goes up to 1 MeV.[78] The PEPSSI sensor has been designed to measure the mass, energy and distribution of charged particles around Pluto, and is also able to differentiate between protons, electrons, and other heavy ions.[79]

Principal investigator: Ralph McNutt Jr., Applied Physics Laboratory

Alice

[edit]

Alice is an ultraviolet imaging spectrometer that is one of two photographic instruments comprising New Horizons' Pluto Exploration Remote Sensing Investigation (PERSI); the other being the Ralph telescope. It resolves 1,024 wavelength bands in the far and extreme ultraviolet (from 50–180 nm), over 32 view fields. Its goal is to determine the composition of Pluto's atmosphere. This Alice instrument is derived from another Alice aboard ESA's Rosetta spacecraft.[78] The instrument has a mass of 4.4 kg and draws 4.4 watts of power. Its primary role is to determine the relative concentrations of various elements and isotopes in Pluto's atmosphere.[80]

Principal investigator: Alan Stern, Southwest Research Institute

In August 2018, NASA confirmed, based on results by Alice on the New Horizons spacecraft, a "hydrogen wall" at the outer edges of the Solar System that was first detected in 1992 by the two Voyager spacecraft.[25][26]

Ralph telescope

[edit]
Ralph—telescope and color camera

The Ralph telescope, 75 mm[81] in aperture, is one of two photographic instruments that make up New Horizons' Pluto Exploration Remote Sensing Investigation (PERSI), with the other being the Alice instrument. Ralph has two separate channels: MVIC (Multispectral Visible Imaging Camera), a visible-light CCD imager with broadband and color channels; and LEISA (Linear Etalon Imaging Spectral Array), a near-infrared imaging spectrometer. LEISA is derived from a similar instrument on the Earth Observing-1 spacecraft. Ralph was named after Alice's husband on The Honeymooners, and was designed after Alice.[82]

On June 23, 2017, NASA announced that it has renamed the LEISA instrument to the "Lisa Hardaway Infrared Mapping Spectrometer" in honor of Lisa Hardaway, the Ralph program manager at Ball Aerospace, who died in January 2017 at age 50.[83]

Principal investigator: Alan Stern, Southwest Research Institute

Venetia Burney Student Dust Counter (VBSDC)

[edit]
VBSDC—Venetia Burney Student Dust Counter

The Venetia Burney Student Dust Counter (VBSDC), built by students at the University of Colorado Boulder, is operating periodically to make dust measurements.[84][85] It consists of a detector panel, about 460 mm × 300 mm (18 in × 12 in), mounted on the anti-solar face of the spacecraft (the ram direction), and an electronics box within the spacecraft. The detector contains fourteen polyvinylidene difluoride (PVDF) panels, twelve science and two reference, which generate voltage when impacted. Effective collecting area is 0.125 m2 (1.35 sq ft). No dust counter has operated past the orbit of Uranus; models of dust in the outer Solar System, especially the Kuiper belt, are speculative. The VBSDC is always turned on measuring the masses of the interplanetary and interstellar dust particles (in the range of nano- and picograms) as they collide with the PVDF panels mounted on the New Horizons spacecraft. The measured data is expected to greatly contribute to the understanding of the dust spectra of the Solar System. The dust spectra can then be compared with those from observations of other stars, giving new clues as to where Earth-like planets can be found in the universe. The dust counter is named for Venetia Burney, who first suggested the name "Pluto" at the age of 11. A thirteen-minute short film about the VBSDC garnered an Emmy Award for student achievement in 2006.[86]

Principal investigator: Mihaly Horanyi, University of Colorado Boulder

Radio Science Experiment (REX)

[edit]

The Radio Science Experiment (REX) used an ultrastable crystal oscillator (essentially a calibrated crystal in a miniature oven) and some additional electronics to conduct radio science investigations using the communications channels. These are small enough to fit on a single card. Because there are two redundant communications subsystems, there are two, identical REX circuit boards.

Principal investigators: Len Tyler and Ivan Linscott, Stanford University

Journey to Pluto

[edit]

Launch

[edit]
Launch of New Horizons. The Atlas V rocket on the launchpad (left) and lift off from Cape Canaveral.

On September 24, 2005, the spacecraft arrived at the Kennedy Space Center on board a C-17 Globemaster III for launch preparations.[87] The launch of New Horizons was originally scheduled for January 11, 2006, but was initially delayed until January 17, 2006, to allow for borescope inspections of the Atlas V's kerosene tank. Further delays related to low cloud ceiling conditions downrange, and high winds and technical difficulties—unrelated to the rocket itself—prevented launch for a further two days.[88][89]

The probe finally lifted off from Pad 41 at Cape Canaveral Air Force Station, Florida, directly south of Space Shuttle Launch Complex 39, at 19:00 UTC on January 19, 2006.[90][91] The Centaur second stage ignited at 19:04:43 UTC and burned for 5 minutes 25 seconds. It reignited at 19:32 UTC and burned for 9 minutes 47 seconds. The ATK Star 48B third stage ignited at 19:42:37 UTC and burned for 1 minute 28 seconds.[92] Combined, these burns successfully sent the probe on a solar-escape trajectory at 16.26 kilometers per second (58,536 km/h; 36,373 mph).[8] New Horizons took only nine hours to pass the Moon's orbit.[93] Although there were backup launch opportunities in February 2006 and February 2007, only the first twenty-three days of the 2006 window permitted the Jupiter flyby. Any launch outside that period would have forced the spacecraft to fly a slower trajectory directly to Pluto, delaying its encounter by five to six years.[94]

The probe was launched by a Lockheed Martin Atlas V 551 rocket, with a third stage added to increase the heliocentric (escape) speed. This was the first launch of the Atlas V 551 configuration, which uses five solid rocket boosters, and the first Atlas V with a third stage. Previous flights had used zero, two, or three solid boosters, but never five. The vehicle, AV-010, weighed 573,160 kilograms (1,263,600 lb) at lift-off,[92] and had earlier been slightly damaged when Hurricane Wilma swept across Florida on October 24, 2005. One of the solid rocket boosters was hit by a door. The booster was replaced with an identical unit, rather than inspecting and requalifying the original.[95]

The launch was dedicated to the memory of launch conductor Daniel Sarokon, who was described by space program officials as one of the most influential people in the history of space travel.[96]

Inner Solar System

[edit]

Trajectory corrections

[edit]

On January 28 and 30, 2006, mission controllers guided the probe through its first trajectory-correction maneuver (TCM), which was divided into two parts (TCM-1A and TCM-1B). The total velocity change of these two corrections was about 18 meters per second (65 km/h; 40 mph). TCM-1 was accurate enough to permit the cancellation of TCM-2, the second of three originally scheduled corrections.[97] On March 9, 2006, controllers performed TCM-3, the last of three scheduled course corrections. The engines burned for 76 seconds, adjusting the spacecraft's velocity by about 1.16 m/s (4.2 km/h; 2.6 mph).[98] Further trajectory maneuvers were not needed until September 25, 2007 (seven months after the Jupiter flyby), when the engines were fired for 15 minutes and 37 seconds, changing the spacecraft's velocity by 2.37 m/s (8.5 km/h; 5.3 mph),[99] followed by another TCM, almost three years later on June 30, 2010, that lasted 35.6 seconds, when New Horizons had already reached the halfway point (in time traveled) to Pluto.[100]

In-flight tests and crossing of Mars orbit

[edit]

During the week of February 20, 2006, controllers conducted initial in-flight tests of three onboard science instruments, the Alice ultraviolet imaging spectrometer, the PEPSSI plasma-sensor, and the LORRI long-range visible-spectrum camera. No scientific measurements or images were taken, but instrument electronics, and in the case of Alice, some electromechanical systems were shown to be functioning correctly.[101]

On April 7, 2006, the spacecraft passed the orbit of Mars, moving at roughly 21 km/s (76,000 km/h; 47,000 mph) away from the Sun at a solar distance of 243 million kilometers.[102][103][104]

Asteroid 132524 APL

[edit]
Asteroid 132524 APL viewed by New Horizons in June 2006
First images of Pluto in September 2006

Because of the need to conserve fuel for possible encounters with Kuiper belt objects subsequent to the Pluto flyby, intentional encounters with objects in the asteroid belt were not planned. After launch, the New Horizons team scanned the spacecraft's trajectory to determine if any asteroids would, by chance, be close enough for observation. In May 2006 it was discovered that New Horizons would pass close to the tiny asteroid 132524 APL on June 13, 2006. Closest approach occurred at 4:05 UTC at a distance of 101,867 km (63,297 mi) (around one quarter of the average Earth-Moon distance). The asteroid was imaged by Ralph (use of LORRI was not possible because of proximity to the Sun), which gave the team a chance to test Ralph's capabilities, and make observations of the asteroid's composition as well as light and phase curves. The asteroid was estimated to be 2.5 km (1.6 mi) in diameter.[105][106][107] The spacecraft successfully tracked the rapidly moving asteroid over June 10–12, 2006.

First Pluto sighting

[edit]

The first images of Pluto from New Horizons were acquired September 21–24, 2006, during a test of LORRI. They were released on November 28, 2006.[108] The images, taken from a distance of approximately 4.2 billion km (2.6 billion mi; 28 AU), confirmed the spacecraft's ability to track distant targets, critical for maneuvering toward Pluto and other Kuiper belt objects.

Jupiter encounter

[edit]
Infrared image of Jupiter by New Horizons

New Horizons used LORRI to take its first photographs of Jupiter on September 4, 2006, from a distance of 291 million kilometers (181 million miles).[109] More detailed exploration of the system began in January 2007 with an infrared image of the moon Callisto, as well as several black-and-white images of Jupiter itself.[110] New Horizons received a gravity assist from Jupiter, with its closest approach at 05:43:40 UTC on February 28, 2007, when it was 2.3 million kilometers (1.4 million miles) from Jupiter. The flyby increased New Horizons' speed by 4 km/s (14,000 km/h; 9,000 mph), accelerating the probe to a velocity of 23 km/s (83,000 km/h; 51,000 mph) relative to the Sun and shortening its voyage to Pluto by three years.[111]

The flyby was the center of a four-month intensive observation campaign lasting from January to June. Being an ever-changing scientific target, Jupiter has been observed intermittently since the end of the Galileo mission in September 2003. Knowledge about Jupiter benefited from the fact that New Horizons' instruments were built using the latest technology, especially in the area of cameras, representing a significant improvement over Galileo's cameras, which were modified versions of Voyager cameras, which, in turn, were modified Mariner cameras. The Jupiter encounter also served as a shakedown and dress rehearsal for the Pluto encounter. Because Jupiter is much closer to Earth than Pluto, the communications link can transmit multiple loadings of the memory buffer; thus the mission returned more data from the Jovian system than it was expected to transmit from Pluto.[112]

One of the main goals during the Jupiter encounter was observing its atmospheric conditions and analyzing the structure and composition of its clouds. Heat-induced lightning strikes in the polar regions and "waves" that indicate violent storm activity were observed and measured. The Little Red Spot, spanning up to 70% of Earth's diameter, was imaged from up close for the first time.[111] Recording from different angles and illumination conditions, New Horizons took detailed images of Jupiter's faint ring system, discovering debris left over from recent collisions within the rings or from other unexplained phenomena. The search for undiscovered moons within the rings showed no results. Travelling through Jupiter's magnetosphere, New Horizons collected valuable particle readings.[111] "Bubbles" of plasma that are thought to be formed from material ejected by the moon Io were noticed in the magnetotail.[113]

Jovian moons

[edit]

The four largest moons of Jupiter were in poor positions for observation; the necessary path of the gravity-assist maneuver meant that New Horizons passed millions of kilometers from any of the Galilean moons. Still, its instruments were intended for small, dim targets, so they were scientifically useful on large, distant moons. Emphasis was put on Jupiter's innermost Galilean moon, Io, whose active volcanoes shoot out tons of material into Jupiter's magnetosphere, and further. Out of eleven observed eruptions, three were seen for the first time. That of Tvashtar reached an altitude of up to 330 km (210 mi). The event gave scientists an unprecedented look into the structure and motion of the rising plume and its subsequent fall back to the surface. Infrared signatures of a further 36 volcanoes were noticed.[111] Callisto's surface was analyzed with LEISA, revealing how lighting and viewing conditions affect infrared spectrum readings of its surface water ice.[114] Minor moons such as Amalthea had their orbit solutions refined. The cameras determined their positions, acting as "reverse optical navigation".

Jovian moons imaged by New Horizons
Io imaged on February 28, 2007. The feature near the north pole of the moon is a 290 km (180 mi) high plume from the volcano Tvashtar.
Europa imaged on February 27, 2007, from a distance of 3.1 million km (1.9 million mi). Image scale is 15 km per pixel (9.3 mi/px).
Ganymede imaged on February 27, 2007, from a distance of 3.5 million km (2.2 million mi). Image scale is 17 km per pixel (11 mi/px).
Callisto imaged on February 27, 2007, from a distance of 4.7 million km (2.9 million mi).
Media related to Photos of Jupiter system by New Horizons at Wikimedia Commons

Outer Solar System

[edit]
Heliocentric positions of the five interstellar probes (squares) and other bodies (circles) until 2020, with launch and flyby dates. Markers denote positions on 1 January of each year, with every fifth year labelled.
Plot 1 is viewed from the north ecliptic pole, to scale.
Plots 2 to 4 are third-angle projections at 20% scale.
In the SVG file, hover over a trajectory or orbit to highlight it and its associated launches and flybys.

After passing Jupiter, New Horizons spent most of its journey towards Pluto in hibernation mode. Redundant components as well as guidance and control systems were shut down to extend their life cycle, decrease operation costs and free the Deep Space Network for other missions.[115] During hibernation mode, the onboard computer monitored the probe's systems and transmitted a signal back to Earth; a "green" code if everything was functioning as expected or a "red" code if mission control's assistance was needed.[115] The probe was activated for about two months a year so that the instruments could be calibrated and the systems checked. The first hibernation mode cycle started on June 28, 2007,[115] the second cycle began on December 16, 2008,[116] the third cycle on August 27, 2009,[117] and the fourth cycle on August 29, 2014, after a 10-week test.[118]

New Horizons crossed the orbit of Saturn on June 8, 2008,[119] and Uranus on March 18, 2011.[120] After astronomers announced the discovery of two new moons in the Pluto system, Kerberos and Styx, mission planners started contemplating the possibility of the probe running into unseen debris and dust left over from ancient collisions between the moons. A study based on 18 months of computer simulations, Earth-based telescope observations and occultations of the Pluto system revealed that the possibility of a catastrophic collision with debris or dust was less than 0.3% on the probe's scheduled course.[121][122] If the hazard increased, New Horizons could have used one of two possible contingency plans, the so-called SHBOTs (Safe Haven by Other Trajectories). Either the probe could have continued on its present trajectory with the antenna facing the incoming particles so the more vital systems would be protected, or it could have positioned its antenna to make a course correction that would take it just 3,000 km (1,900 mi) from the surface of Pluto where it was expected that the atmospheric drag would have cleaned the surrounding space of possible debris.[122]

While in hibernation mode in July 2012, New Horizons started gathering scientific data with SWAP, PEPSSI and VBSDC. Although it was originally planned to activate just the VBSDC, other instruments were powered on in order to collect valuable heliospheric data. Before activating the other two instruments, ground tests were conducted to make sure that the expanded data gathering in this phase of the mission would not limit available energy, memory and fuel in the future and that all systems were functioning during the flyby.[123] The first set of data was transmitted in January 2013 during a three-week activation from hibernation. The command and data handling software was updated to address the problem of computer resets.[124]

Possible Neptune trojan targets

[edit]

Other possible targets were Neptune trojans. The probe's trajectory to Pluto passed near Neptune's trailing Lagrange point ("L5"), which may host hundreds of bodies in 1:1 resonance. In late 2013, New Horizons passed within 1.2 AU (180 million km; 110 million mi) of the high-inclination L5 Neptune trojan 2011 HM102,[125] which was discovered shortly before by the New Horizons KBO Search task, a survey to find additional distant objects for New Horizons to fly by after its 2015 encounter with Pluto. At that range, 2011 HM102 would have been bright enough to be detectable by New Horizons' LORRI instrument; however, the New Horizons team eventually decided that they would not target 2011 HM102 for observations because the preparations for the Pluto approach took precedence.[126] On August 25, 2014, New Horizons crossed the orbit of Neptune, exactly 25 years after the planet was visited by the Voyager 2 probe.[127] This was the last major planet orbit crossing before the Pluto flyby. At the time, the spacecraft was 3.99 billion km (2.48 billion mi; 26.7 AU) away from Neptune and 4.51 billion km (2.80 billion mi; 30.1 AU) from the Sun.

Observations of Pluto and Charon 2013–14

[edit]

Images from July 1 to 3, 2013, by LORRI were the first by the probe to resolve Pluto and Charon as separate objects.[128] On July 14, 2014, mission controllers performed a sixth trajectory-correction maneuver (TCM) since its launch to enable the craft to reach Pluto.[129] Between July 19–24, 2014, New Horizons' LORRI snapped 12 images of Charon revolving around Pluto, covering almost one full rotation at distances ranging from about 429 to 422 million km (267 to 262 million mi).[130] In August 2014, astronomers made high-precision measurements of Pluto's location and orbit around the Sun using the Atacama Large Millimeter/submillimeter Array (ALMA), an array of radio telescopes located in Chile, to help NASA's New Horizons spacecraft accurately home in on Pluto.[131] On December 6, 2014, mission controllers sent a signal for the craft to "wake up" from its final Pluto-approach hibernation and begin regular operations. The craft's response that it was "awake" reached Earth on December 7, 2014, at 02:30 UTC.[132][133][134]

Pluto approach

[edit]
Pluto and Charon photographed on April 9, 2015, (left) by Ralph and on June 29, 2015, (right) by LORRI.

Distant-encounter operations at Pluto began on January 4, 2015.[135] On this date, images of the targets with the onboard LORRI imager plus the Ralph telescope were only a few pixels in width. Investigators began taking Pluto images and background starfield images to assist mission navigators in the design of course-correcting engine maneuvers that would precisely modify the trajectory of New Horizons to aim the approach.[136]

On February 12, 2015, NASA released new images of Pluto (taken from January 25 to 31) from the approaching probe.[137][138] New Horizons was more than 203 million km (126 million mi) away from Pluto when it began taking the photos, which showed Pluto and its largest moon, Charon. The exposure time was too short to see Pluto's smaller, much fainter moons.

Investigators compiled a series of images of the moons Nix and Hydra taken from January 27 through February 8, 2015, beginning at a range of 201 million km (125 million mi).[139] Pluto and Charon appear as a single overexposed object at the center. The right side image has been processed to remove the background starfield. The other two, even smaller moons—Kerberos and Styx—were seen on photos taken on April 25.[140] Starting on May 11, a hazard search was performed, looking for unknown objects that could be a danger to the spacecraft, such as rings or hitherto undiscovered moons, which could then possibly be avoided by a course change.[141] No rings or additional moons were found.

Also in regard to the approach phase during January 2015, on August 21, 2012, the team announced that they would spend mission time attempting long-range observations of the Kuiper belt object temporarily designated VNH0004 (now designated 2011 KW48), when the object was at a distance of 75 million km (0.50 AU; 47 million mi) from New Horizons.[142] The object would be too distant to resolve surface features or take spectroscopy, but it would be able to make observations that cannot be made from Earth, namely a phase curve and a search for small moons. A second object was planned to be observed in June 2015, and a third in September after the flyby; the team hoped to observe a dozen such objects through 2018.[142] On April 15, 2015, Pluto was imaged showing a possible polar cap.[143]

Software glitch

[edit]

On July 4, 2015, New Horizons experienced a software anomaly and went into safe mode, preventing the spacecraft from performing scientific observations until engineers could resolve the problem.[144][145] On July 5, NASA announced that the problem was determined to be a timing flaw in a command sequence used to prepare the spacecraft for its flyby, and the spacecraft would resume scheduled science operations on July 7. The science observations lost because of the anomaly were judged to have no impact on the mission's main objectives and minimal impact on other objectives.[146]

The timing flaw consisted of performing two tasks simultaneously—compressing previously acquired data to release space for more data, and making a second copy of the approach command sequence—that together overloaded the spacecraft's primary computer. After the overload was detected, the spacecraft performed as designed: it switched from the primary computer to the backup computer, entered safe mode, and sent a distress call back to Earth. The distress call was received the afternoon of July 4 and alerted engineers that they needed to contact the spacecraft to get more information and resolve the issue. The resolution was that the problem happened as part of preparations for the approach, and was not expected to happen again because no similar tasks were planned for the remainder of the encounter.[146][147]

Pluto system encounter

[edit]
Alan Stern and the New Horizons team celebrate after the spacecraft successfully completed its flyby of Pluto.

The closest approach of the New Horizons spacecraft to Pluto occurred at 11:49 UTC on July 14, 2015, at a range of 12,472 km (7,750 mi) from the surface[148] and 13,658 km (8,487 mi) from the center of Pluto. Telemetry data confirming a successful flyby and a healthy spacecraft was received on Earth from the vicinity of the Pluto system on July 15, 2015, 00:52:37 UTC,[149] after 22 hours of planned radio silence due to the spacecraft being pointed towards the Pluto system. Mission managers estimated a one in 10,000 chance that debris could have destroyed the probe or its communication-systems during the flyby, preventing it from sending data to Earth.[150] The first details of the encounter were received the next day, but the download of the complete data set through the 2 kbps data downlink took just over 15 months.[18]

Objectives

[edit]

The mission's science objectives were grouped in three distinct priorities. The "primary objectives" were required. The "secondary objectives" were expected to be met but were not demanded. The "tertiary objectives" were desired. These objectives could have been skipped in favor of the above objectives. An objective to measure any magnetic field of Pluto was dropped, due to mass and the expense associated with including a magnetometer on the spacecraft. Instead, SWAP and PEPSSI could indirectly detect magnetic fields around Pluto.[151]

  • Primary objectives (required)
    • Characterize the global geology and morphology of Pluto and Charon
    • Map chemical compositions of Pluto and Charon surfaces
    • Characterize the neutral (non-ionized) atmosphere of Pluto and its escape rate
  • Secondary objectives (expected)
  • Tertiary objectives (desired)
    • Characterize the energetic particle environment at Pluto and Charon
    • Refine bulk parameters (radii, masses) and orbits of Pluto and Charon
    • Search for additional moons and any rings

"The New Horizons flyby of the Pluto system was fully successful, meeting and in many cases exceeding, the Pluto objectives set out for it by NASA and the National Academy of Sciences."[152]

Flyby details

[edit]
Pluto's "encounter hemisphere" viewed by New Horizons on July 14, 2015
Pluto's Charon-facing opposing hemisphere viewed on July 11, 2015
Animation of New Horizons' flyby of Pluto in Eyes on the Solar System.

On July 14, 2015, at 11:50 UTC, New Horizons made its closest approach to Pluto, passing within 12,500 km (7,800 mi) at a speed of 13.78 km/s (49,600 km/h; 30,800 mph), while also coming as close as 28,800 km (17,900 mi) to Charon. Starting 3.2 days prior, the spacecraft mapped Pluto and Charon with 40 km (25 mi) resolution, enabling coverage of all sides. Close-range imaging was conducted twice daily to monitor for surface changes, such as snowfall or cryovolcanism. During the flyby, LORRI captured images with up to 50 m (160 ft) resolution, MVIC created four-color global maps at 1.6 km (1 mi) resolution, and LEISA obtained near-infrared hyperspectral maps at resolutions ranging from 7 km/px (4.3 mi/px) globally to 0.6 km/px (0.37 mi/px) for selected areas.

Patterns of blue-gray ridges and reddish material observed in the Tartarus Dorsa region on July 14, 2015

Meanwhile, Alice characterized the atmosphere, both by emissions of atmospheric molecules (airglow), and by dimming of background stars as they pass behind Pluto (occultation). During and after closest approach, SWAP and PEPSSI sampled the high atmosphere and its effects on the solar wind. VBSDC searched for dust, inferring meteoroid collision rates and any invisible rings. REX performed active and passive radio science. The communications dish on Earth measured the disappearance and reappearance of the radio occultation signal as the probe flew by behind Pluto. The results resolved Pluto's diameter (by their timing) and atmospheric density and composition (by their weakening and strengthening pattern). (Alice can perform similar occultations, using sunlight instead of radio beacons.) Previous missions had the spacecraft transmit through the atmosphere, to Earth ("downlink"). Pluto's mass and mass distribution were evaluated by the gravitational tug on the spacecraft. As the spacecraft speeds up and slows down, the radio signal exhibited a Doppler shift. The Doppler shift was measured by comparison with the ultrastable oscillator in the communications electronics.

Reflected sunlight from Charon allowed some imaging observations of the nightside. Backlighting by the Sun gave an opportunity to highlight any rings or atmospheric hazes. REX performed radiometry of the nightside.

Satellite observations

[edit]

New Horizons' best spatial resolution of the small satellites is 330 m per pixel (1,080 ft/px) at Nix, 780 m/px (2,560 ft/px) at Hydra, and approximately 1.8 km/px (1.1 mi/px) at Kerberos and Styx. Estimates for the dimensions of these bodies are: Nix at 49.8 × 33.2 × 31.1 km (30.9 × 20.6 × 19.3 mi); Hydra at 50.9 × 36.1 × 30.9 km (31.6 × 22.4 × 19.2 mi); Kerberos at 19 × 10 × 9 km (11.8 × 6.2 × 5.6 mi); and Styx at 16 × 9 × 8 km (9.9 × 5.6 × 5.0 mi).[153]

Initial predictions envisioned Kerberos as a relatively large and massive object whose dark surface led to it having a faint reflection. This proved to be wrong as images obtained by New Horizons on July 14 and sent back to Earth in October 2015 revealed that Kerberos was smaller in size, 19 km (12 mi) across with a highly reflective surface suggesting the presence of relatively clean water ice similarly to the rest of Pluto's smaller moons.[154]

Satellites of Pluto imaged by New Horizons
Media related to Photos of Pluto system by New Horizons at Wikimedia Commons

Post-Pluto events

[edit]
View of Pluto as New Horizons left the system, catching the Sun's rays passing through Pluto's atmosphere, forming a ring

Soon after the Pluto flyby, in July 2015, New Horizons reported that the spacecraft was healthy, its flight path was within the margins, and science data of the Pluto–Charon system had been recorded.[155][156] The spacecraft's immediate task was to begin returning the 6.25 gigabytes of information collected.[18] The free-space path loss at its distance of 4.5 light-hours (3 billion km or 20 AU or 1.9 billion mi) is approximately 303 dB at 7 GHz. Using the high gain antenna and transmitting at full power, the signal from EIRP is +83 dBm, and at this distance, the signal reaching Earth is −220 dBm. The received signal level (RSL) using one, un-arrayed Deep Space Network antenna with 72 dBi of forward gain equals −148 dBm.[157] Because of the extremely low RSL, it could only transmit data at 1 to 2 kilobits per second.[158]

By March 30, 2016, about nine months after the flyby, New Horizons reached the halfway point of transmitting this data.[159] The transfer was completed on October 25, 2016, at 21:48 UTC, when the last piece of data—part of a Pluto–Charon observation sequence by the Ralph/LEISA imager—was received by the Johns Hopkins University Applied Physics Laboratory.[18][160]

As of November 2018, at a distance of 43 AU (6.43 billion km; 4.00 billion mi) from the Sun and 0.4 AU (60 million km; 37 million mi) from 486958 Arrokoth,[161] New Horizons was heading in the direction of the constellation Sagittarius[162] at 14.10 km/s (8.76 mi/s; 2.97 AU/a) relative to the Sun.[161] The brightness of the Sun from the spacecraft was magnitude −18.5.[162]

On April 17, 2021, New Horizons reached a distance of 50 AU from the Sun, while remaining fully operational.[163]

Mission extension

[edit]
Big picture: from the inner Solar System to the Oort cloud with the Kuiper belt in between

The New Horizons team requested, and received, a mission extension through 2021 to explore additional Kuiper belt objects (KBOs). Funding was secured on July 1, 2016.[164] During this Kuiper Belt Extended Mission (KEM) the spacecraft performed a close fly-by of 486958 Arrokoth and will conduct more distant observations of an additional two dozen objects,[165][164][166] and possibly make a fly-by of another KBO.[citation needed]

Kuiper belt object mission

[edit]

Target background

[edit]

Mission planners searched for one or more additional Kuiper belt objects (KBOs) of the order of 50–100 km (30–60 mi) in diameter as targets for flybys similar to the spacecraft's Plutonian encounter. However, despite the large population of KBOs, many factors limited the number of possible targets. Because the flight path was determined by the Pluto flyby, and the probe only had 33 kg (73 lb) of hydrazine propellant remaining, the object to be visited needed to be within a cone of less than a degree's width extending from Pluto. The target also needed to be within 55 AU, because beyond 55 AU, the communications link becomes too weak, and the RTG power output decays significantly enough to hinder observations.[167] Desirable KBOs are well over 50 km (30 mi) in diameter, neutral in color (to contrast with the reddish Pluto), and, if possible, have a moon that imparts a wobble.[citation needed]

[edit]
Trajectory of New Horizons and other nearby Kuiper belt objects

In 2011, mission scientists started the New Horizons KBO Search, a dedicated survey for suitable KBOs using ground telescopes. Large ground telescopes with wide-field cameras, notably the twin 6.5-meter Magellan Telescopes in Chile, the 8.2-meter Subaru Observatory in Hawaii and the Canada–France–Hawaii Telescope[125][168] were used to search for potential targets. By participating in a citizen-science project called Ice Hunters the public helped to scan telescopic images for possible suitable mission candidates.[169][170][171][172][173] The ground-based search resulted in the discovery of about 143 KBOs of potential interest,[174] but none of these were close enough to the flight path of New Horizons.[168] Only the Hubble Space Telescope was deemed likely to find a suitable target in time for a successful KBO mission.[175] On June 16, 2014, time on Hubble was granted for a search.[176] Hubble has a much greater ability to find suitable KBOs than ground telescopes. The probability that a target for New Horizons would be found was estimated beforehand at about 95%.[177]

Suitable KBOs

[edit]
486958 Arrokoth, the announced target for the Kuiper belt object mission

On October 15, 2014, it was revealed that Hubble's search had uncovered three potential targets,[178][179][180][181][182] temporarily designated PT1 ("potential target 1"), PT2 and PT3 by the New Horizons team. PT1 was eventually chosen as the target and would be named 486958 Arrokoth.

All objects had estimated diameters in the 30–55 km (19–34 mi) range and were too small to be seen by ground telescopes. The targets were at distances from the Sun ranging from 43 to 44 AU, which would put the encounters in the 2018–2019 period.[179] The initial estimated probabilities that these objects were reachable within New Horizons' fuel budget were 100%, 7%, and 97%, respectively.[179] All were members of the "cold" (low-inclination, low-eccentricity) classical Kuiper belt objects, and thus were very different from Pluto.

PT1 (given the temporary designation "1110113Y" on the HST web site[183]), the most favorably situated object, had a magnitude of 26.8, is 30–45 km (19–28 mi) in diameter, and was encountered in January 2019.[184] A course change to reach it required about 35% of New Horizons' available trajectory-adjustment fuel supply. A mission to PT3 was in some ways preferable, in that it is brighter and therefore probably larger than PT1, but the greater fuel requirements to reach it would have left less for maneuvering and unforeseen events.[179]

Once sufficient orbital information was provided, the Minor Planet Center gave provisional designations to the three target KBOs: 2014 MU69 (PT1' later 486958 Arrokoth), 2014 OS393 (PT2), and 2014 PN70 (PT3). By the fall of 2014, a possible fourth target, 2014 MT69, had been eliminated by follow-up observations. PT2 was out of the running before the Pluto flyby.[185][186]

KBO selection

[edit]

On August 28, 2015, 486958 Arrokoth (then known as (486958) 2014 MU69 and nicknamed Ultima Thule) (PT1) was chosen as the flyby target. The necessary course adjustment was performed with four engine firings between October 22 and November 4, 2015.[187][188] The flyby occurred on January 1, 2019, at 00:33 UTC.[189][190]

Observations of other KBOs

[edit]

Aside from its flyby of 486958 Arrokoth, the extended mission for New Horizons calls for the spacecraft to conduct observations of, and look for ring systems around, between 25 and 35 different KBOs.[191] In addition, it will continue to study the gas, dust and plasma composition of the Kuiper belt before the mission extension ends in 2021.[165][166][needs update]

On November 2, 2015, New Horizons imaged KBO 15810 Arawn with the LORRI instrument from 280 million km away (170 million mi; 1.9 AU).[192] This KBO was again imaged by the LORRI instrument on April 7–8, 2016, from a distance of 111 million km (69 million mi; 0.74 AU). The new images allowed the science team to further refine the location of 15810 Arawn to within 1,000 km (620 mi) and to determine its rotational period of 5.47 hours.[193][194]

In July 2016, the LORRI camera captured some distant images of Quaoar from 2.1 billion km away (1.3 billion mi; 14 AU); the oblique view will complement Earth-based observations to study the object's light-scattering properties.[195]

On December 5, 2017, when New Horizons was 40.9 AU from Earth, a calibration image of the Wishing Well cluster marked the most distant image ever taken by a spacecraft (breaking the 27-year record set by Voyager 1's famous Pale Blue Dot). Two hours later, New Horizons surpassed its own record, imaging the Kuiper belt objects 2012 HZ84 and 2012 HE85 from a distance of 0.50 and 0.34 AU, respectively. These were the closest images taken of a Kuiper belt object besides Pluto and Arrokoth as of February 2018.[196][197]

The dwarf planet Haumea was observed from afar by the New Horizons spacecraft in October 2007, January 2017, and May 2020, from distances of 49 AU, 59 AU, and 63 AU, respectively. New Horizons has observed the dwarf planets Eris (2020), Haumea (2007, 2017, 2020), Makemake (2007, 2017), and Quaoar (2016, 2017, 2019), as well as the large KBOs Ixion (2016), Máni (2016, 2017, 2019), and 2014 OE394 (2017, 2018). It also observed Neptune's largest moon Triton (which shares similarities with Pluto and Eris) in 2019.[198]

Extended mission imaging targets
15810 Arawn in April 2016
50000 Quaoar in July 2016 at a distance of about 14 AU[195]
Calibration image of the Wishing Well cluster from December 2017
False-color image of 2012 HZ84 from December 2017
False-color image of 2012 HE85 from December 2017
Media related to Photos of Kuiper belt objects by New Horizons at Wikimedia Commons

By December 2023, New Horizons had discovered a total of about 100 KBOs, and flown close enough to about 20 of them to capture characteristics such as shape, rotational period, possible moons, and surface composition. In addition, since 2021, Canadian researchers had been able to use machine learning software to speed up identification processes of potential KBO targets for a third flyby, cutting weeks-long efforts to hours-long.[198][199]

Encounter with Arrokoth

[edit]
Animation of New Horizons' flyby of Arrokoth in Eyes on the Solar System.
Animation of New Horizons's trajectory from January 19, 2006, to December 30, 2030
   New Horizons  ·   486958 Arrokoth ·   Earth ·   132524 APL ·   Jupiter  ·   Pluto
New Horizons image of Arrokoth

Objectives

[edit]

Science objectives of the flyby included characterizing the geology and morphology of Arrokoth[200][201] and mapping the surface composition (by searching for ammonia, carbon monoxide, methane, and water ice). Searches will be conducted for orbiting moonlets, a coma, rings and the surrounding environment.[202] Additional objectives include:[203]

  • Mapping the surface geology to learn how it formed and evolved
  • Measuring the surface temperature
  • Mapping the 3-D surface topography and surface composition to learn how it is similar to and different from comets such as 67P/Churyumov–Gerasimenko and dwarf planets such as Pluto
  • Searching for any signs of activity, such as a cloud-like coma
  • Searching for and studying any satellites or rings
  • Measuring or constraining the mass

Targeting maneuvers

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Arrokoth is the first object to be targeted for a flyby that was discovered after the spacecraft was launched.[204] New Horizons was planned to come within 3,500 km (2,200 mi) of Arrokoth, three times closer than the spacecraft's earlier encounter with Pluto. Images with a resolution of up to 30 m (98 ft) per pixel were expected.[205]

The new mission began on October 22, 2015, when New Horizons carried out the first in a series of four initial targeting maneuvers designed to send it towards Arrokoth. The maneuver, which started at approximately 19:50 UTC and used two of the spacecraft's small hydrazine-fueled thrusters, lasted approximately 16 minutes and changed the spacecraft's trajectory by about 10 meters per second (33 ft/s). The remaining three targeting maneuvers took place on October 25, October 28, and November 4, 2015.[206][207]

Approach phase

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The craft was brought out of its hibernation at approximately 00:33 UTC SCET on June 5, 2018 (06:12 UTC ERT, Earth-Received Time),[a] in order to prepare for the approach phase.[209][210] After verifying its health status, the spacecraft transitioned from a spin-stabilized mode to a three-axis-stabilized mode on August 13, 2018. The official approach phase began on August 16, 2018, and continued through December 24, 2018.[211]

New Horizons made its first detection of Arrokoth on August 16, 2018, from a distance of 172 million km (107 million mi). At that time, Arrokoth was visible at magnitude 20 against a crowded stellar background in the direction of the constellation Sagittarius.[212][213]

Flyby

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The Core phase began a week before the encounter and continued for two days after the encounter. The spacecraft flew by the object at a speed of 51,500 km/h (32,000 mph; 14.3 km/s) and within 3,500 km (2,200 mi).[214] The majority of the science data was collected within 48 hours of the closest approach in a phase called the Inner Core.[211] Closest approach occurred January 1, 2019, at 05:33 UTC[215] SCET at which point the probe was 43.4 AU from the Sun.[216] At this distance, the one-way transit time for radio signals between Earth and New Horizons was six hours.[202] Confirmation that the craft had succeeded in filling its digital recorders occurred when data arrived on Earth ten hours later, at 15:29 UTC.[217]

Data download

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After the encounter, preliminary, high-priority data was sent to Earth on January 1 and 2, 2019. On January 9, New Horizons returned to a spin-stabilized mode to prepare sending the remainder of its data back to Earth.[211] This download was expected to take 20 months at a data rate of 1–2 kilobits per second.[218] As of July 2022, approximately 10% of the data was still left to be received.[219]

Post-Arrokoth events

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Parallax of Proxima Centauri as observed from New Horizons and Earth.[220]

In April 2020, New Horizons was used in conjunction with telescopes on Earth to take pictures of nearby stars Proxima Centauri and Wolf 359; the images from each vantage point – over 6.4 billion km (4 billion miles) apart – were compared to produce "the first demonstration of an easily observable stellar parallax."[220]

Images taken by the LORRI camera while New Horizons was 42 to 45 AU from the Sun were used to measure the cosmic optical background, the visible light analog of the cosmic microwave background, in seven high galactic latitude fields. At that distance New Horizons saw a sky ten times darker than the sky seen by the Hubble Space Telescope because of the absence of diffuse background sky brightness from the zodiacal light in the inner solar system. These measurements indicate that the total amount of light emitted by all galaxies at ultraviolet and visible wavelengths may be lower than previously thought.[221][222]

New Horizons' position[161]

The spacecraft reached a distance of 50 AU (7.5 billion km; 4.6 billion mi) on April 17, 2021, at 12:42 UTC, a feat performed only four times before, by Pioneer 10, Pioneer 11, Voyager 1, and Voyager 2. Voyager 1 is the farthest spacecraft from the Sun, more than 152 AU (22.7 billion km; 14.1 billion mi) away when New Horizons reached its landmark in 2021.[163] The support team continued to use the spacecraft in 2021 to study the heliospheric environment (plasma, dust and gas) and to study other Kuiper Belt objects.[223]

The All-sky New Horizons Alice Lyα maps in ecliptic coordinates centered on the anti-Sun direction, and the lower map is in Galactic coordinates. The ~90,000 stars in the M. A. Velez et al. (2024) catalog are overlaid as black dots, where the size of the dot is proportional to the logarithm of the expected Alice count rate from each star. The map in Galactic coordinates indicates the outlines of four of the important LISM clouds ("LIC," in red; "Aql," in green; "Blue," in blue; and "G," in tan).[224]

In 2025, the first map of all Lyman-Alpha emissions in the Milky Way galaxy was published, based on New Horizons observations.[224]

Plans

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After the spacecraft passed Arrokoth, the instruments continue to have enough power to be operational until the 2030s.

Team leader Alan Stern stated there is potential for a third flyby in the 2020s at the outer edges of the Kuiper belt.[225][226] This depends on a suitable Kuiper belt object being found or confirmed close enough to the spacecraft's current trajectory. Since May 2020, the New Horizons team has been using time on the Subaru Telescope to look for suitable candidates within the spacecraft's proximity. As of June 2024, no suitable targets have been found. Beginning in fiscal year 2025, New Horizons will focus on specific heliophysics data, as stated by NASA in September 2023. It will remain available for a flyby of a different target until it leaves the Kuiper belt in 2028.[227]

New Horizons may also take a picture of Earth from its distance in the Kuiper belt, but only after completing all planned KBO flybys and imaging Uranus and Neptune.[228][229] This is because pointing a camera towards Earth could cause the camera to be damaged by sunlight,[230] as none of New Horizons' cameras have an active shutter mechanism.[231][232]

Speed

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Speed and distance from the Sun

New Horizons has been called "the fastest spacecraft ever launched"[7] because it left Earth at 16.26 kilometers per second (58,536 km/h; 36,373 mph).[8][9] It is also the first spacecraft launched directly into a solar escape trajectory, which requires an approximate speed while near Earth of 16.5 km/s (59,000 km/h; 37,000 mph),[b] plus additional delta-v to cover air and gravity drag, all to be provided by the launch vehicle. As of May 2, 2024, the spacecraft is 58.80 AU (8.796 billion km; 5.466 billion mi) from the Sun traveling at 13.68 kilometres per second (49,200 km/h; 30,600 mph).[233]

However, it is not the fastest spacecraft to leave the Solar System. As of July 2023, this record is held by Voyager 1, traveling at 16.985 km/s (61,146 km/h; 37,994 mph) relative to the Sun.[162] Voyager 1 attained greater hyperbolic excess velocity than New Horizons due to gravity assists by Jupiter and Saturn. When New Horizons reaches the distance of 100 AU (15 billion km; 9.3 billion mi), it will be traveling at about 13 km/s (47,000 km/h; 29,000 mph), around 4 km/s (14,000 km/h; 8,900 mph) slower than Voyager 1 at that distance.[234] The Parker Solar Probe can also be measured as the fastest object, because of its orbital speed relative to the Sun at perihelion: 191 km/s (690,000 km/h; 430,000 mph).[235][c] Because it remains in solar orbit, its specific orbital energy relative to the Sun is lower than New Horizons and other artificial objects escaping the Solar System.

New Horizons' Star 48B third stage is also on a hyperbolic escape trajectory from the Solar System and reached Jupiter before the New Horizons spacecraft; it was expected to cross Pluto's orbit on October 15, 2015.[237] Because it was not in controlled flight, it did not receive the correct gravity assist and passed within 200 million km (120 million mi) of Pluto.[237] The Centaur second stage did not achieve solar escape velocity and remains in a heliocentric orbit.[238]

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Images of the launch

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The Atlas V 551 rocket, used to launch New Horizons, being processed a month before launch.
View of Cape Canaveral Launch Complex 41, with the Atlas V carrying New Horizons on the pad.
Distant view of Cape Canaveral during the launch of New Horizons on January 19, 2006.
NASA TV footage of New Horizons' launch from Cape Canaveral. (4:00)

Videos

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See also

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Notes

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References

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Further reading

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
New Horizons is an interplanetary spacecraft launched by NASA on January 19, 2006, as part of the agency's New Frontiers program, designed to conduct the first close-up exploration of Pluto and its moons while also investigating the Kuiper Belt, a distant region of icy bodies beyond Neptune.[1] Built and operated by the Johns Hopkins Applied Physics Laboratory (APL), the probe traveled at speeds exceeding 36,000 miles per hour (58,000 km/h) after launch aboard an Atlas V rocket from Cape Canaveral, Florida, making it one of the fastest spacecraft ever to leave Earth.[2] The mission's primary objectives included mapping Pluto's surface, studying its thin atmosphere, and analyzing its five known moons—Charon, Styx, Nix, Kerberos, and Hydra—to gain insights into the solar system's formation and evolution.[1] During its journey, New Horizons performed a gravity-assist flyby of Jupiter in February 2007, capturing detailed images of the planet and its moons Io, Europa, and Ganymede, which helped refine the spacecraft's trajectory and provided valuable data on Jupiter's magnetosphere.[2] The spacecraft is equipped with a suite of seven scientific instruments, including the Long Range Reconnaissance Imager (LORRI) for high-resolution photography, the Ralph imager and spectrometer for surface composition analysis, the Alice ultraviolet spectrometer for atmospheric studies, and particle detectors like SWAP and PEPSSI to measure solar wind interactions.[1] On July 14, 2015, New Horizons achieved its landmark goal with a flyby of Pluto at a distance of approximately 7,800 miles (12,500 km), revealing a complex world with nitrogen ice plains, towering mountains, and a hazy atmosphere, fundamentally reshaping our understanding of dwarf planets.[2] The mission continued into the Kuiper Belt, culminating in a historic encounter with the object Arrokoth (provisionally designated 2014 MU69, nicknamed "Ultima Thule") on January 1, 2019—the most distant flyby of any celestial body at over 4 billion miles (6.5 billion km) from Earth—which provided the first close-up views of a pristine planetesimal from the solar system's early history.[1] As of February 2026, New Horizons is in a prolonged hibernation phase in the Kuiper Belt at approximately 65 AU (about 9.7 billion km) from Earth, traveling through the Kuiper Belt at about 300 million miles (480 million km) per year, powered by a radioisotope thermoelectric generator using plutonium-238.[3][4] It is continuing passive data collection with select instruments while conserving power; the hibernation began in August 2025 and is planned to end in June 2026 pending budget approval, with the spacecraft remaining healthy and on its extended trajectory through the outer solar system.[3] It now focuses on heliophysics observations of particles and plasma in the outer solar system, astrophysical studies of the interstellar medium, and searches for additional Kuiper Belt objects, transmitting data back to Earth at rates as low as 1 kilobit per second due to its vast distance.[1] The mission has returned over 50 gigabits of scientific data, contributing to more than 1,200 peer-reviewed publications and advancing knowledge of the solar system's edge.[2]

Overview and Objectives

Mission Goals

The New Horizons mission, selected by NASA in 2001 as the first project under its New Frontiers Program, aimed to conduct the first close-up reconnaissance of the Pluto-Charon system.[5][6] The mission goals were later expanded to include the moons Nix and Hydra, discovered in 2005. This primary objective focused on mapping surfaces, analyzing compositions, and measuring physical properties to understand the geology and atmospheres of these distant bodies. Following the Pluto encounter, the mission extended to explore the Kuiper Belt, targeting flybys of small Kuiper Belt Objects (KBOs) to investigate their origins and compositions as remnants of the solar system's formation.[1] Secondary goals included a gravity-assist flyby of Jupiter to study its atmosphere, rings, and moons, such as Io and Europa, providing valuable data on Jovian dynamics while accelerating the spacecraft toward Pluto.[7][8] Additionally, the mission encompassed broad surveys of KBOs to characterize their diversity, sizes, and surface properties, contributing to insights into the outer solar system's evolution.[9][8] Launched on January 19, 2006, aboard an Atlas V rocket, New Horizons reached Jupiter in February 2007, arrived at Pluto on July 14, 2015, and performed a flyby of the KBO Arrokoth (2014 MU69) on January 1, 2019.[1][10] The mission continues with ongoing KBO observations and heliophysics measurements, projected to extend through 2029 as the spacecraft exits the Kuiper Belt.[11] The total mission cost was approximately $700 million, covering development, launch, operations, and data analysis.[8]

Scientific Objectives

The New Horizons mission's scientific objectives for Pluto center on characterizing its surface composition, which includes mapping distributions of volatiles such as nitrogen, methane, and carbon monoxide ices, as well as investigating geological features like potential cryovolcanism and impact craters to understand its evolutionary history.[12] The mission aims to determine the structure of Pluto's atmosphere, including its thermal profile, haze layers, and escape rate of atmospheric constituents into space. These investigations address fundamental questions about how Pluto retains its atmosphere against solar wind stripping and whether internal heat sources could sustain dynamic surface processes.[12][1] For Charon, Pluto's largest moon, the objectives focus on mapping its water-ice-dominated surface composition and global geology to identify tectonic features, resurfacing events, and a possible ancient cryovolcanic history, which could reveal tidal interactions with Pluto that have shaped its orbital evolution.[12] Investigations of the smaller moons, Nix, Hydra, Kerberos, and Styx, seek to assess their surface compositions, likely mixtures of water ice and organics, and to study formation mechanisms, such as whether they originated from a giant impact between Pluto and Charon or through capture processes. The objectives for the smaller moons were initially for Nix and Hydra, and later extended to include Kerberos (discovered 2011) and Styx (discovered 2012).[12] These goals include evaluating tidal evolution models and surface features like albedo variations to infer their dynamical stability within the Pluto system.[12] In the Kuiper Belt, New Horizons targets the diversity of Kuiper Belt Objects (KBOs) by studying their sizes, albedos, and surface compositions during flybys, such as that of Arrokoth (2014 MU69), to probe the primordial building blocks of the outer solar system.[1] These observations aim to test hypotheses on KBO formation from the solar nebula, including binary formation rates and color variations that indicate compositional gradients.[12] During its 2007 Jupiter flyby, the mission's objectives include measuring atmospheric dynamics, such as wind patterns and storm evolution in Jupiter's bands, and characterizing the magnetosphere's plasma interactions with the ionosphere to understand magnetic field generation and auroral phenomena.[12] Additional goals encompass studying volcanic activity on Io through plume monitoring and compositional mapping of its surface, providing context for outer planet moon geology.[12] Instruments like the Long Range Reconnaissance Imager contribute to these objectives by enabling high-resolution imaging across targets.[12] Overall, these objectives test broader hypotheses on planetary migration, such as the Nice model, by examining how Pluto's orbital resonance with Neptune and KBO distributions reflect giant planet rearrangements early in solar system history, informing the evolution of the outer solar system.[12]

Development and Design

Project History

The New Horizons mission originated from NASA's Announcement of Opportunity (AO-OSS-01) issued on January 20, 2001, soliciting proposals for a Pluto-Kuiper Belt flyby mission as the inaugural project under the New Frontiers program, which aimed to conduct medium-class planetary science investigations with a cost cap of $506 million in FY 2001 dollars.[12] The proposal, emphasizing a fast-track reconnaissance of Pluto and potential Kuiper Belt objects, was submitted on April 6, 2001, as one of several initial entries in this competitive process.[12] In June 2001, NASA narrowed the field to two concepts for further study, selecting New Horizons on November 29, 2001, following peer review, to fulfill the program's first mission slot dedicated to outer solar system exploration.[12] Led by Principal Investigator Dr. Alan Stern of the Southwest Research Institute (SwRI), the project drew on expertise from a multidisciplinary team, with spacecraft development and management handled by the Johns Hopkins University Applied Physics Laboratory (APL) as the primary contractor.[12] SwRI served as the science payload integrator, while additional support came from institutions like Ball Aerospace for key instruments and international collaborators on specific components, such as contributions to the Alice ultraviolet spectrometer from European teams.[13] A notable educational outreach element was the Venetia Burney Student Dust Counter (VBSDC), the first planetary science instrument fully designed, built, calibrated, and operated by university students, primarily from the University of Colorado Laboratory for Atmospheric and Space Physics, highlighting grassroots involvement in the mission's instrumentation.[14] Following selection, the project entered Phase A (concept and technology development) from June to October 2001, transitioning to full-scale development after NASA approval and funding in March 2003.[15] The design and preliminary engineering phase spanned 2001 to 2004, focusing on a compact, spin-stabilized spacecraft powered by a radioisotope thermoelectric generator (RTG) to enable operations beyond the reach of solar arrays. Construction and integration occurred primarily from 2004 to mid-2005 at APL facilities in Laurel, Maryland, incorporating the science payload and propulsion systems.[12] Environmental testing, including vibration, thermal vacuum, and electromagnetic compatibility trials, took place from late 2005 to early 2006, addressing the mission's demanding requirements for reliability over a decade-long cruise.[16] Development faced significant challenges, including adherence to the New Frontiers cost constraints amid NASA's broader fiscal pressures in the early 2000s, which necessitated efficient management and innovative engineering to stay within the approximately $565 million development budget including launch vehicle.[17][18] The use of plutonium-238 in the RTG required rigorous nuclear safety reviews by the Department of Energy, NASA, and the White House Office of Science and Technology Policy, culminating in approval with an estimated 1-in-360 risk of release during launch accidents.[12] Precise navigation demands for a high-speed flyby of a distant, poorly characterized target like Pluto also drove extensive simulation efforts during the design phase.[16] In preparation for launch, final assembly and systems integration were completed at APL in summer 2005, after which the spacecraft underwent final checkout and fueling. The fully integrated New Horizons was shipped to Cape Canaveral Air Force Station, Florida, in September 2005 via secure transport, arriving for mating with the Atlas V launch vehicle in December 2005 at Space Launch Complex 41.[19] This culminated in the January 19, 2006, liftoff, marking the end of the primary development phase.[12]

Spacecraft Architecture

The New Horizons spacecraft features a compact, piano-sized main body measuring approximately 0.7 meters in height, 2.1 meters in length, and 2.7 meters across its widest point, with a total launch mass of 478 kilograms including 77 kilograms of hydrazine propellant.[20][8] The structure consists of an aluminum central cylinder supporting lightweight honeycomb-core panels with ultra-thin face sheets, covered in multilayer insulation blankets for thermal protection, enabling operation in the harsh deep-space environment.[21] This design balances the spacecraft for spin stabilization at about 5 revolutions per minute during cruise phases, while a despin mechanism using 12 small hydrazine thrusters (each providing 0.8 Newtons of thrust) allows transition to three-axis stabilized mode for precise observations.[20] To ensure reliability over the mission's decade-long duration, the avionics incorporate significant redundancy, including dual processors, backup electronics for major subsystems, and cross-strapped communication interfaces for fault tolerance.[21][22] The central computing core, housed in a radiation-hardened Integrated Electronics Module with a 12-MHz Mongoose V processor, manages command handling, data processing, and subsystem coordination.[20] Instruments and payloads are integrated directly onto the body panels without deployable elements, with the seven-science-instrument suite mounted around the central cylinder; a 2.1-meter high-gain parabolic antenna deploys post-launch for communication via NASA's Deep Space Network, supplemented by medium- and low-gain antennas for redundancy.[21][20] A poignant human element is included aboard: a small canister containing approximately one ounce of the cremated ashes of astronomer Clyde Tombaugh, discoverer of Pluto, mounted on the inner upper deck as a symbolic tribute to the mission's origins.[23]

Key Subsystems

The New Horizons spacecraft's propulsion and attitude control system relies on 16 hydrazine thrusters—four larger ones providing 4.4 Newtons of thrust for trajectory corrections and twelve smaller ones delivering 0.8 Newtons for fine pointing and spin rate adjustments—along with 77 kilograms of hydrazine propellant stored in a helium-pressurized titanium tank.[21] The system enables spin stabilization at 5 revolutions per minute during cruise phases for stability and switches to three-axis control using the thrusters for precise instrument pointing during planetary encounters, without the use of reaction wheels.[21] Power for the spacecraft is generated by a single radioisotope thermoelectric generator (RTG) fueled by approximately 11 kilograms of plutonium-238 dioxide, which produced about 240 watts electrical power at launch in 2006 and degraded to roughly 200 watts by the 2015 Pluto flyby due to an annual decay rate of approximately 4 watts.[8] The RTG outputs 30 volts direct current to the spacecraft bus, with no batteries included, and excess heat is managed to support thermal needs.[21] The flight computer consists of two redundant radiation-hardened Mongoose-V processors operating at 12 MHz in a 32-bit architecture, housed within the integrated electronics module to handle command processing, autonomous sequencing, and subsystem coordination in the deep-space radiation environment.[21] Telecommunications are facilitated by a 2.1-meter high-gain parabolic antenna for primary downlink, supplemented by a 0.3-meter medium-gain antenna and two low-gain antennas for backup and acquisition, all operating in the X-band frequency around 8.4 GHz.[24] The system features two 12-watt traveling-wave tube amplifiers for transmission, supporting data rates from approximately 1 kilobit per second at Pluto distances to up to 38 kilobits per second nearer the inner solar system.[24] Thermal control is achieved primarily through passive methods, including 18 layers of multilayer insulation blankets to minimize heat loss, along with electric heaters that activate automatically and variable louvers to reject excess heat from the RTG, maintaining critical components within a 10–30°C (50–86°F) operating range.[21] Data handling is managed by two redundant solid-state recorders, each with 8 gigabytes of capacity, which store science observations, engineering telemetry, and playback sequences before transmission to Earth, with the flight computer overseeing compression and prioritization.[21]

Instruments

Imaging and Mapping Instruments

The imaging and mapping instruments on the New Horizons spacecraft, primarily the Long-Range Reconnaissance Imager (LORRI) and the Ralph Multispectral Imager and Spectrometer, were designed to capture high-resolution images and spectral data of distant targets like Pluto and its moons, enabling detailed surface mapping and compositional analysis from afar.[25] These instruments provided panchromatic and multispectral views essential for characterizing geological features and atmospheric interactions without the need for landing.[26] LORRI is a panchromatic telescope featuring a 20.8 cm diameter primary mirror in a Ritchey-Chrétien design, delivering high-resolution imaging with a narrow field of view of 0.29 degrees and pixel scales of 4.95 μrad.[27] Coupled to a 1024 × 1024 pixel CCD detector, it operates without filters to maximize sensitivity in visible wavelengths (roughly 400-900 nm), achieving resolutions as fine as 1 km per pixel during the approach to Pluto from distances of several million kilometers.[28] This configuration allowed LORRI to serve as the spacecraft's primary tool for contextual and high-fidelity mapping, capturing sharp details of surface morphology even under low-light conditions typical of the outer solar system.[25] The Ralph instrument complements LORRI with a 75 mm aperture telescope that feeds light to two integrated channels: the Multispectral Visible Imaging Camera (MVIC) for visible-light imaging and the Linear Etalon Imaging Spectral Array (LEISA) for near-infrared spectroscopy.[29] MVIC employs seven linear CCD arrays—three panchromatic and four in color bands (blue, red, and two near-infrared)—to produce color and panchromatic maps, operating in scan mode via time-delay integration (TDI) for efficient coverage of extended surfaces or in framing mode for targeted snapshots.[30] The panchromatic mode, often referred to as Pancam, provides broad-context imaging at resolutions suitable for global mapping, while the color channels enable differentiation of surface units based on albedo and spectral signatures.[25] LEISA, integrated within Ralph, functions as a short-wavelength infrared (1.25-2.50 μm) imaging spectrometer using a pushbroom scan technique with a wedged etalon to disperse light across 256 spectral channels, allowing for the mapping of volatile ices such as water, methane, and nitrogen, as well as organic hazes like tholins.[31] This capability was crucial for identifying compositional variations across planetary surfaces, with the instrument's design ensuring robust performance at the low power of 7.1 W and mass of 10.5 kg for the entire Ralph package.[29] Together, these modes facilitated coordinated observations where MVIC provided morphological context and LEISA added spectroscopic depth, all synchronized with the spacecraft's pointing system for precise targeting.[26]

Particle and Plasma Instruments

The New Horizons spacecraft carries two primary instruments dedicated to measuring charged particles and plasma environments: the Solar Wind Around Pluto (SWAP) instrument and the Pluto Energetic Particle Spectrometer Science Investigation (PEPSSI). These instruments enable detailed characterization of the solar wind's interaction with Pluto's extended atmosphere, including the detection of pickup ions and the assessment of plasma dynamics in the distant heliosphere. SWAP focuses on lower-energy solar wind plasma, while PEPSSI targets higher-energy particles, providing complementary data on the overall particle populations around the Pluto system.[32][33] The SWAP instrument, developed by Southwest Research Institute, is an electrostatic analyzer designed to measure ions and electrons from the solar wind, with an energy range spanning approximately 35 eV to 7.5 keV for ions. It incorporates a retarding potential analyzer (RPA) for precise velocity measurements down to 0-2000 V, paired with electrostatic deflectors and a top-hat electrostatic analyzer (ESA) that achieves an energy resolution of better than 9% full width at half maximum (FWHM) above 2 keV. SWAP's field of view covers 276° × 10°, allowing nearly full-sky monitoring as the spacecraft spins, and it employs channel electron multipliers with a carbon foil for coincidence detection to suppress noise and enhance sensitivity to low fluxes typical at 30 AU, down to about 0.01 cm⁻³. Calibration at the SwRI Ion Calibration Facility using beams from <500 eV to 51 keV confirmed its geometric factor of 1.8 × 10⁻³ cm² sr eV/eV, enabling accurate derivation of solar wind speed, density, and temperature for studies of atmospheric mass loading and potential magnetospheric boundaries at Pluto.[32][34] Complementing SWAP, PEPSSI is a compact time-of-flight (TOF) spectrometer, approximately 7.6 cm in diameter and 2.5 cm thick, built by the Johns Hopkins Applied Physics Laboratory with a mass of 1.475 kg and power consumption of 2.49 W. It detects ions from ~20 eV to 1 MeV and electrons from 25 keV to 500 keV, providing energy spectra and compositional information across a 160° × 12° fan-shaped field of view divided into six sectors for directional mapping. The TOF system features a 6 cm drift path with polyimide foils that generate secondary electrons detected by microchannel plates, yielding a resolution of <1 ns FWHM and enabling species discrimination—such as protons (mass resolution <2 AMU), CNO-group ions (<5 AMU), and heavier elements—through combined TOF and energy measurements via solid-state detectors. Ground calibration at APL using linear accelerators for 30-170 keV protons and oxygen ions, along with in-flight verification during the Jupiter flyby, established a geometric factor of ≥0.1 cm² sr for ions and processing rates up to 10³ events/s, allowing PEPSSI to map energetic particle distributions and pickup ions indicative of Pluto's atmospheric escape rate.[33][35] Together, SWAP and PEPSSI provide critical insights into plasma interactions, with SWAP's Faraday-cup-like RPA offering bulk solar wind parameters and PEPSSI's TOF enabling detailed ion tracing, though their sensitivities are optimized for the sparse particle fluxes beyond 30 AU. These measurements support broader understanding of how solar wind plasma shapes Pluto's ionosphere and exosphere.[32][33]

Spectroscopic and Dust Instruments

The Alice ultraviolet imaging spectrograph on the New Horizons spacecraft is a lightweight (4.4 kg), low-power (4.4 W) instrument designed to probe the composition and structure of planetary atmospheres through far-ultraviolet spectroscopy.[36] Operating in the 52–187 nm wavelength range with a spectral resolution of 3–6 Å full width at half maximum (FWHM), Alice determines the relative abundances of key gases such as N₂, CO, and CH₄ in Pluto's atmosphere, maps its vertical density and temperature profiles, assesses haze optical depth, and measures atmospheric escape rates.[37] During the 2007 Jupiter flyby, it conducted calibration observations and studied Jupiter's upper atmosphere and auroral emissions, providing insights into its composition and dynamics.[36] Alice's optical design features an off-axis telescope feeding a Rowland-circle spectrograph with dual gratings and detectors, enabling both high-resolution solar occultation measurements and broadband airglow observations.[36] Its slitless airglow channel, with a 0.1° × 4.0° field of view and spatial resolution of approximately 0.6°, allows for extended mapping of atmospheric emissions without a physical slit, facilitating efficient coverage of Pluto's hazy atmosphere and escape processes during the 2015 encounter.[36] This configuration, with an effective area up to 0.30 cm² in the 1000–1100 Å band, supports the instrument's primary role in characterizing neutral atmospheric species and their interactions with solar radiation.[36] The Venetia Burney Student Dust Counter (VBSDC), the first student-built scientific instrument to fly on a NASA planetary mission, detects interstellar and interplanetary dust particles along the spacecraft's trajectory using piezoelectric sensors.[38] Developed by students at the University of Colorado's Laboratory for Atmospheric and Space Physics under professional oversight, VBSDC employs thin polyvinylidene fluoride (PVDF) films that generate electrical pulses upon dust impacts, measuring particles with masses greater than 10⁻¹² g—corresponding to radii exceeding approximately 0.58 μm for typical densities of 2.5 g/cm³, or effectively >1 μm in size.[39][40] With a total sensitive area of about 0.1 m² oriented toward the spacecraft's ram direction, it continuously monitors dust flux from launch in 2006 through the Pluto encounter and beyond, mapping spatial variations in dust density across the outer solar system.[39] Early VBSDC results from 2006–2010 revealed interplanetary dust fluxes of roughly 2.5 × 10⁻⁴ m⁻² s⁻¹ between 6.8 and 15.5 AU, consistent with prior missions like Pioneer and Voyager, while also confirming interstellar dust detections inside Jupiter's orbit out to 15.5 AU.[40] This ongoing dataset, analyzed by student teams, provides critical context for dust origins in the Kuiper Belt and interstellar medium, with operations extending well past the Pluto flyby to support extended mission objectives.[38]

Radio and Auxiliary Experiments

The Radio Science Experiment (REX) on the New Horizons spacecraft leveraged the X-band telecommunications system to conduct radio occultation observations during the July 14, 2015, flyby of Pluto, enabling measurements of the dwarf planet's neutral atmosphere and searches for ionospheric structure.[41] This experiment transmitted a 7.2 GHz uplink signal from NASA's Deep Space Network antennas on Earth, with power levels of 10–30 kW, which was received and processed by the spacecraft's receiver as Pluto occulted the line of sight twice—once at ingress (sunset) and once at egress (sunrise).[42] Perturbations in the signal's phase and amplitude, caused by refractive bending in Pluto's atmosphere, were analyzed using an Abel inversion transform to derive vertical profiles of temperature, pressure, and density, achieving a vertical resolution of approximately 1–2 km in the lower atmosphere.[41] Additionally, REX measured Pluto's thermal emission at 4.2 cm wavelength during occultation to estimate disk-averaged brightness temperatures.[42] Key findings from the REX occultations revealed a surface pressure of 11 ± 1 μbar and a surface temperature of 45 ± 3 K at egress, with evidence of a strong temperature inversion in the lower atmosphere rising to about 70 K at altitudes above 20 km. The atmospheric profiles showed near-symmetry between ingress and egress, consistent with nitrogen sublimation-driven dynamics, and indicated a lapse rate of 6.4 ± 0.9 K km⁻¹ near the surface at ingress, decreasing to 3.4 ± 0.9 K km⁻¹ higher up. No ionosphere was detected around Pluto, with REX placing an upper limit on peak electron density of less than 1000 cm⁻³ at the terminator, below model predictions for photoionization-driven plasma.[43] These measurements provided the first direct constraints on Pluto's atmospheric structure down to the surface, confirming a thinner and colder lower atmosphere than pre-encounter models anticipated. Auxiliary components of the radio experiment included an ultrastable oscillator (USO) integrated into the spacecraft's radio hardware, which maintained frequency stability to σ_y(τ) ≈ 2 × 10⁻¹³ at 1000 s integration time, enabling high-precision Doppler tracking for gravitational studies.[42] By analyzing two-way Doppler shifts in the radio signals during the approach and flyby, REX determined the total mass of the Pluto-Charon system to an expected accuracy of 0.01%, while also refining the individual masses and orbits of Pluto and Charon through combined tracking and occultation data.[41] This capability supported broader objectives in characterizing the system's bulk properties, though actual precision was influenced by spacecraft thruster firings during the encounter.[44]

Launch and Early Cruise

Launch Sequence

The New Horizons spacecraft lifted off on January 19, 2006, at 19:00 UTC from Space Launch Complex 41 at Cape Canaveral Air Force Station in Florida, aboard an Atlas V 551 launch vehicle configured with five solid rocket boosters and a Star 48B third-stage solid rocket motor.[1][7] The launch sequence proceeded nominally, with the solid rocket boosters separating 2 minutes after liftoff and the Atlas V first stage burning for about 4.5 minutes to reach an initial suborbital trajectory. The Centaur upper stage then ignited for its first burn of 9 minutes to achieve a circular parking orbit at approximately 185 km altitude, followed by a coast phase and a second burn lasting 5.5 minutes to inject the stack into a hyperbolic escape trajectory. Roughly 66 minutes after liftoff, the Star 48B third stage ignited for 87 seconds, accelerating the spacecraft to an Earth-relative velocity of 16.26 km/s (36,400 mph or 58,500 km/h)—the fastest launch speed ever attained by a spacecraft—and placing it on a direct path toward a Jupiter gravity assist en route to the Pluto system.[1][7][45] Spacecraft separation from the expended third stage occurred about 1 hour and 15 minutes after liftoff, at which point New Horizons inherited a nominal spin rate of around 60 RPM from the stage for initial stabilization. A yo-yo despin mechanism was then deployed to reduce the spin to 5 RPM, enabling activation of the star scanner for attitude determination and the commencement of three-axis stabilized operations as needed. The first telemetry signal was acquired approximately 1.5 hours post-launch by ground stations, verifying successful separation, power-up of the radioisotope thermoelectric generators, and overall spacecraft health with no significant anomalies reported during the immediate post-separation phase.[45][8][46]

Inner Solar System Phase

Following its launch on January 19, 2006, from Cape Canaveral, Florida, the New Horizons spacecraft entered the inner solar system phase, a critical period spanning January to June 2006 focused on trajectory refinement, system verification, and initial science opportunities en route to the Jupiter gravity assist. During this time, the mission team executed navigation operations to align the spacecraft with its outbound path, including preparations for solar conjunction effects on communications, though the primary conjunction blackout occurred later in November 2006. The phase emphasized stabilizing the high-velocity escape trajectory, which reached approximately 36,400 mph (58,500 km/h) shortly after launch, while monitoring environmental conditions in the warmer inner heliosphere.[1][47] Trajectory correction maneuvers (TCMs) were essential to correct minor launch dispersions and ensure precise Jupiter targeting, with a total pre-Jupiter delta-V budget allocated around 60 m/s across planned burns. TCM-1, split into two parts for calibration and correction, occurred on January 28 (TCM-1A, ~5 m/s) and January 30 (TCM-1B, ~13.3 m/s), addressing initial errors and totaling about 18 m/s; its accuracy allowed cancellation of the subsequent TCM-2. TCM-3 followed on March 9 with a smaller adjustment (1.16 m/s), serving as the final pre-Jupiter correction and collectively achieving the required alignment with minimal propellant use. These maneuvers utilized the spacecraft's hydrazine propulsion system, demonstrating its reliability for fine course adjustments.[48][16][47] In-flight tests dominated the phase, with comprehensive instrument checkouts conducted to verify functionality after launch stresses. All seven science instruments, including the Long Range Reconnaissance Imager (LORRI), Ralph multispectral imager, and plasma analyzers like SWAP and PEPSSI, underwent activation, calibration, and performance assessments between late January and May, confirming operational readiness without major anomalies. The radioisotope thermoelectric generators (RTGs) were monitored closely, with early cruise data showing power output exceeding specifications at approximately 240 W, validating long-term decay predictions and thermal management. LORRI captured its first images of Earth and the Moon in late January 2006 from ~1 million km, providing initial calibration data on pointing accuracy and image quality. The spacecraft's automated thermal control system, crucial in the inner solar system's elevated solar flux, encountered minor heater glitches resolved via onboard software updates to optimize power distribution.[49][50][51][52] New Horizons crossed the orbit of Mars (at 1.5 AU from the Sun) on April 7, 2006, marking the fastest spacecraft to pass this milestone since Voyager 2 in 1977 and entering the main asteroid belt. Later in the phase, on June 13, 2006, the spacecraft performed an opportunistic flyby of asteroid 132524 APL (discovered in 2002 and named after the mission's lead institution) at a closest approach of 101,867 km (63,297 mi). This event tested the Ralph instrument's visible and infrared capabilities, yielding ~20 images and spectra that revealed the asteroid's composition, including a reddish surface indicative of organic materials, while serving as a rehearsal for distant target observations. No significant challenges arose beyond routine thermal adjustments, affirming the spacecraft's robustness for the outer solar system journey.[1][1][53]

Jupiter Gravity Assist

The New Horizons spacecraft executed its Jupiter gravity assist on February 28, 2007, achieving closest approach to the planet at a distance of 2.3 million kilometers (approximately 32 Jovian radii) at 05:43:40 UT.[54] This maneuver utilized Jupiter's immense gravitational field to increase the spacecraft's heliocentric velocity by nearly 4 km/s, equivalent to about 14,000 km/h, thereby shortening the journey to the Pluto system by more than three years and advancing the arrival date from 2019 to 2015.[52] The flyby trajectory passed south of Jupiter's equator at -8 degrees latitude, with the spacecraft traveling at 21 km/s relative to the planet, enabling a comprehensive four-month observation campaign from January to June 2007.[55] During the encounter, New Horizons conducted over 700 separate observations, capturing more than 700 images of Jupiter's atmospheric features, including its swirling cloud bands, the evolving Little Red Spot storm, and subtle magnetospheric interactions.[56] The Long Range Reconnaissance Imager (LORRI) and Ralph multispectral imager/spectrometer provided high-resolution visible and infrared imagery, revealing morphological changes in Jupiter's belts and zones, wind speeds exceeding 150 m/s in the Little Red Spot, and new insights into the planet's faint ring system and dust tori.[54][57] The Solar Wind Around Pluto (SWAP) and Pluto Energetic Particle Spectrometer Science Investigation (PEPSSI) instruments measured energetic particles and solar wind interactions, mapping auroral activity in Jupiter's polar regions and traversing the magnetotail to study plasma dynamics.[54] Observations of Jupiter's moons included detailed monitoring of Io's volcanic eruptions, with LORRI detecting multiple active plumes and lava flows; infrared scans of Europa's surface hinted at subsurface ocean influences through thermal anomalies; and ultraviolet imaging of Ganymede's auroral emissions.[58][59] The Jupiter flyby served as a critical rehearsal for the Pluto encounter, fully validating all seven science instruments under operational conditions and confirming the spacecraft's pointing accuracy and data downlink capabilities.[52] Scientifically, the data contributed significant advances to Jovian studies, including the first detection of lightning strikes in Jupiter's polar auroral zones using radio emissions, enhanced understanding of atmospheric circulation via storm tracking, and refined models of the magnetosphere's structure from particle distributions.[54] These results, transmitted back to Earth over subsequent months, enriched the global Jupiter research community prior to the more distant Pluto mission phase.[1]

Approach to Pluto System

Trajectory Corrections

Following the Jupiter gravity assist in February 2007, the New Horizons spacecraft underwent a series of trajectory correction maneuvers (TCMs) to refine its ballistic path toward the Pluto system, ensuring precise alignment for the 2015 flyby. These maneuvers were essential to correct minor errors from launch and the gravity assist, using the spacecraft's hydrazine-fueled propulsion system for small velocity changes.[47] The post-Jupiter phase relied exclusively on these TCMs for trajectory control, as no additional planetary encounters were planned.[60] A total of seven major TCMs were performed after the Jupiter flyby, contributing to an overall mission delta-V of approximately 25 m/s across nine TCMs from launch to Pluto arrival—far below the 131 m/s budgeted for the primary mission. This efficient navigation conserved a significant portion of the initial 77 kg hydrazine propellant load, leaving about 47 kg (roughly 60-70%) available after the Pluto encounter to enable the extended Kuiper Belt mission, including targeting a distant flyby object.[61][47] The propulsion setup featured four 4.4 N delta-V thrusters for primary adjustments, supplemented by smaller 0.9 N attitude control thrusters when needed, operating in a blow-down mode without pressurization.[61] Key TCMs included an early post-Jupiter adjustment on September 25, 2007, which set the spacecraft on a refined trajectory toward Pluto. Later maneuvers, such as TCM-15 on July 15, 2014 (delta-V of 1.08 m/s) and TCM-15B2 on March 10, 2015 (1.14 m/s via a 93-second burn), further honed the aim point based on accumulating navigation data. Navigation combined Deep Space Network radio tracking for range and Doppler measurements with onboard optical navigation campaigns; the Long Range Reconnaissance Imager (LORRI) captured images of Pluto and Charon starting at distances of several million kilometers, allowing detection of Charon's position relative to Pluto for precise orbit determination and trajectory updates. Over 850 LORRI images and supporting Multicolor Visible Imaging Camera (MVIC) observations refined the ephemeris, achieving flyby accuracy within kilometers.[1][61][62][63] During the cruise, the spacecraft received software updates to bolster autonomous operations, including enhanced fault detection and recovery capabilities via a rule-based expert system. In July 2015, near the Pluto approach, a timing conflict in the command sequence during image data compression and command loading caused the primary computer to overload, triggering safe mode entry; the team resolved it within days by switching to the backup computer and reloading commands, with no impact on the encounter timeline or objectives.[64][65][66]

Outer Solar System Cruise

Following the Jupiter gravity assist in February 2007, New Horizons entered its outer solar system cruise phase, a low-activity period extending through 2013 that focused on preserving spacecraft resources during the long journey to Pluto. This phase, spanning approximately six years, involved minimal operations to counteract the gradual decay of the radioisotope thermoelectric generator (RTG), which supplied about 210 watts at the start but declined by roughly 1.7 watts annually due to plutonium-238 decay. Onboard power management systems maintained bus voltage at 30 volts by shunting excess energy as waste heat, ensuring sufficient allocation for critical functions like telecommunications and thermal control while most instruments remained dormant.[52][67] To minimize wear on electronics and reduce ground operations, the spacecraft pioneered routine hibernation for NASA deep-space missions, entering 18 such periods from mid-2007 to late 2014, totaling 1,873 days or about two-thirds of the flight time to Pluto. Each hibernation lasted 36 to 202 days, with the first commencing on July 5, 2007, after initial post-Jupiter activities; during these intervals, only essential systems operated, sending a weekly beacon tone for health monitoring. The spacecraft awoke 2-3 times annually for checkouts lasting several weeks, involving engineering assessments, instrument calibrations, data downlink, and minor trajectory corrections to align with the Pluto encounter—such adjustments totaled less than 100 meters per second in delta-v over the cruise. Hibernation entries and exits were automated, with daily engineering telemetry collected via the spacecraft's fault protection to detect anomalies early.[68][69][68] Distant observations during this phase began yielding science data, including the first detection of Pluto's largest moon, Charon, on July 1-3, 2013, using the Long Range Reconnaissance Imager (LORRI) at a spacecraft-to-Pluto distance of 550 million miles (880 million kilometers). These six 0.1-second exposures resolved Charon as a faint companion at the predicted position relative to Pluto, 35 years after its discovery from Earth-based telescopes, and confirmed the spacecraft's optical navigation accuracy. Earlier LORRI imaging had captured Pluto as an unresolved point source, but this marked the onset of resolved Pluto system monitoring. The mission also targeted other outer solar system features, such as color imaging of Uranus—including its rings—via the Multispectral Visible Imaging Camera (MVIC) to probe forward-scattering properties at high phase angles unavailable to Earth observers. Additionally, ground-based searches tied to New Horizons identified Neptune Trojans like 2011 HM102 in the L5 region, but none were selected as flyby targets due to incompatible orbital geometries.[70][54][71]

Initial Pluto Observations

As New Horizons approached the Pluto system, its observations transitioned from distant, low-resolution imaging to detailed pre-encounter mapping, spanning roughly from mid-2013 to early 2015. Initial images in July 2013 captured the first detection of Charon as a separated companion using the Long Range Reconnaissance Imager (LORRI), marking the start of resolved observations of Pluto's largest moon at distances exceeding 2 billion kilometers. By April 2015, at approximately 114 million kilometers from Pluto, the spacecraft's cameras began systematic mapping, achieving resolutions around 570 km per pixel and revealing basic surface contrasts on both Pluto and Charon under approach lighting conditions. Instrument rehearsals during this period tested the Ralph Multispectral Visible Imaging Camera (MVIC) and LORRI for color and panchromatic imaging, building toward higher resolutions of about 80 km per pixel by early July 2015 as the spacecraft closed to within 16 million kilometers.[72] Key images from this phase highlighted emerging surface features, including a color view in April 2015 from 113 million kilometers that first showed Pluto's reddish hue and subtle albedo variations, hinting at diverse terrains, with Charon appearing as a resolved disk for the first time. Optical navigation campaigns, initiated in January 2015, utilized LORRI to acquire targeted images of Pluto and its moons against star fields, enabling precise trajectory refinements through centroid measurements and improving positional accuracy to within kilometers. These campaigns, combined with instrument checkouts and simulated flyby sequences, prioritized data collection for geologic mapping and atmospheric scouting, while ground teams at the Deep Space Network coordinated downlinks to manage the spacecraft's limited 2 kilobits-per-second bandwidth. Early discoveries included contrasts in Charon's surface brightness, revealing darker equatorial regions and brighter poles in approach sunlight, providing initial insights into its icy composition.[73][74] The intensifying observation schedule posed significant challenges, particularly the rapidly increasing data volume as resolutions improved and observation sequences multiplied. By early 2015, daily imaging campaigns generated gigabytes of raw data, necessitating onboard compression and selective prioritization—favoring navigation and high-priority science over redundant frames—to fit within storage limits of the spacecraft's 8 gigabyte solid-state recorder. Teams pre-loaded observation commands to ensure uninterrupted approach activities. These efforts culminated in a robust dataset that refined Pluto's ephemeris and set the stage for the July encounter.[49]

Pluto System Encounter

Encounter Objectives

The Pluto system encounter objectives centered on achieving the first detailed reconnaissance of the dwarf planet and its moons, with a focus on high-resolution global mapping of Pluto and Charon's surfaces to characterize their geology and morphology. Atmospheric profiling of Pluto was a key priority, including measurements of its composition, structure, and escape rate to understand volatile transport and loss processes. Satellite characterization encompassed imaging and compositional analysis of Charon, Nix, Hydra, Kerberos, and Styx to assess their formation and evolution within the system. These core goals built on the mission's broader aim to place Pluto in context among icy bodies, drawing from pre-encounter ground-based and Hubble observations.[75] Prioritized measurements targeted specific phenomena, such as the detailed composition of Pluto's nitrogen-dominated ice plains using multispectral imaging and infrared spectroscopy to identify ices like water, methane, and carbon monoxide. The atmospheric escape rate was to be quantified through ultraviolet spectroscopy and energetic particle detection, revealing Jeans escape and potential ion pickup by the solar wind. Internal structure investigations relied on the Radio Science Experiment (REX), which planned radio occultations during entry and exit to probe atmospheric density profiles down to the surface and infer Pluto's and Charon's mass distributions and possible subsurface oceans. These selections emphasized transformative insights over routine surveys, with required observations ensuring baseline data even if secondary goals were curtailed.[75][1] The observation sequence comprised over 900 commands uploaded to the spacecraft, executing more than 380 distinct observation sequences across a nine-day encounter phase, with a high-priority subset scheduled during the closest approach on July 14, 2015, to capture riskier, high-resolution data within the 12,500 km flyby distance. These commands coordinated multiple instruments simultaneously, such as the Long Range Reconnaissance Imager (LORRI) for panchromatic mapping and the Alice ultraviolet spectrograph for atmospheric limb scans, while prioritizing safe spacecraft orientation.[75] Contingencies included pre-planned hazard avoidance maneuvers based on approach-phase imaging from LORRI, which detected no significant debris but allowed for trajectory tweaks up to July 1, 2015; backup sequences like simplified high-gain antenna pointing or reduced observation loads were prepared to protect the spacecraft from potential rings or satellites.[75] Mission operations were coordinated from the Johns Hopkins Applied Physics Laboratory (APL) in Laurel, Maryland, with real-time commanding via NASA's Deep Space Network and science team input from Southwest Research Institute; the spacecraft recorded approximately 50 GB of compressed science data on its dual 8 GB solid-state recorders during the core flyby, prioritizing immediate storage of irreplaceable close-approach observations before downlink began.[75]

Flyby Timeline

The New Horizons spacecraft's approach to the Pluto system intensified in the weeks leading up to the flyby, with the approach phase formally beginning in January 2015 to allow for optical navigation and hazard assessment.[49] By early July, the spacecraft entered the Pluto system's particle environment on July 7, 2015, at 05:18 UTC, when the PEPSSI instrument began detecting charged particles, marking the start of in-situ measurements of the local plasma.[49] Navigation teams conducted final hazard checks using LORRI images taken as close as 1.25 million km on July 11, confirming no major debris fields or trajectory deviations that would require adjustments, allowing the mission to proceed on its nominal path refined through prior trajectory corrections.[63][61] The closest approach to Pluto occurred on July 14, 2015, at 11:49:57 UTC, when the spacecraft passed 12,500 km above the surface at a relative speed of 13.78 km/s.[49] During this 22-hour core imaging period centered on closest approach, New Horizons operated in blackout mode, ceasing communications with Earth from approximately 20:17 UTC on July 13 to 20:52 UTC on July 14 to maximize science data collection, including high-resolution imaging sequences that captured Pluto at resolutions down to 77 meters per pixel.[76] Key events included the REX radio science experiment's occultation of Pluto's atmosphere starting at 12:14 UTC, measuring temperature and density profiles as the spacecraft passed behind the dwarf planet from Earth's view, followed by Charon's occultation at around 13:45 UTC.[49] Instruments ran at high data rates during this phase, generating over 50 gigabits of observations stored onboard for later transmission.[77] In the departure phase over the following weeks, the spacecraft continued remote sensing of Pluto and its moons while reorienting for downlink, avoiding any entry into safe mode despite pre-flyby concerns from a minor anomaly earlier in July.[65] The initial post-flyby signal was reacquired at 20:52 UTC on July 14, with the first engineering data confirming nominal operations downlinked shortly thereafter at rates up to 1 kbps via the high-gain antenna.[76] Subsequent high-volume science data transmission began in earnest by late July, prioritizing low-resolution images and spectra before the full dataset over the next year.[77]

Pluto and Moon Observations

During its flyby of the Pluto system, NASA's New Horizons spacecraft captured detailed images revealing Pluto's surface as a geologically diverse world, dominated by the expansive Sputnik Planitia, a smooth nitrogen ice plain forming the western half of the heart-shaped Tombaugh Regio. This vast basin, spanning approximately 1,000 kilometers across and filled with at least 4 kilometers of nitrogen-dominated ice, exhibits cellular convection patterns driven by solid-state convection and possible internal heat sources, along with flowing glaciers and thousands of small pits indicative of sublimation processes.[78] Adjacent to Sputnik Planitia lie rugged water-ice mountains rising up to 3.5 kilometers high, contrasting with darker, cratered highlands like Cthulhu Macula, which showcase a mix of volatile ices, tholins, and ancient impact features, highlighting Pluto's complex tectonic and erosional history.[79] Pluto's thin atmosphere, primarily composed of nitrogen with traces of methane and hydrocarbons, extends to altitudes exceeding 1,000 kilometers and is characterized by approximately 20 distinct haze layers of organic tholin particles that scatter blue light and influence surface chemistry. Observations indicate a surface temperature of about 45 K, with the upper atmosphere significantly colder—around 65–68 K—than pre-flyby models predicted, leading to a reduced nitrogen escape rate of roughly 10^{27} molecules per second, which challenges understandings of Pluto's long-term atmospheric retention.[80] Among Pluto's moons, Charon exhibited a striking reddish polar cap known as Mordor Macula, likely formed by the deposition and photochemical processing of hydrocarbons from Pluto's escaping atmosphere, covering a region rich in tholins. The moon's surface also features an extensive equatorial belt of canyons, some reaching depths of 7–10 kilometers and spanning over 1,600 kilometers, interpreted as evidence of ancient tectonic extension possibly linked to the freezing of a subsurface ocean. The smaller moons—Nix, Hydra, Kerberos, and Styx—appear as irregular, elongated bodies with dimensions ranging from 10 to 65 kilometers, high geometric albedos of 50–90 percent, and surfaces dominated by water ice, suggesting origins as captured Kuiper Belt debris or remnants of collisional formation.[81] Integrated analyses of New Horizons data point to ongoing active geology on Pluto, including cryovolcanism, glacial resurfacing, and volatile transport cycles that renew much of the surface over geological timescales, powered by residual formation heat and tidal interactions with Charon. On Charon, the canyon systems and wrinkle ridges provide evidence for a past global subsurface ocean that expanded and froze, fracturing the icy crust in a process akin to Europa's tectonics, though current activity appears limited.[78][79] The encounter generated over 50 gigabits of raw data across multiple instruments, equivalent to about 6.25 gigabytes, which was fully transmitted to Earth by October 2016 and subsequently processed into high-resolution geologic maps, atmospheric models, and compositional analyses.[82][83]

Extended Mission in Kuiper Belt

KBO Target Selection Process

Following the successful Pluto flyby in July 2015, the New Horizons team initiated a dedicated search for Kuiper Belt Objects (KBOs) suitable for a post-encounter flyby, beginning ground-based observations in 2011 to identify candidates within the spacecraft's post-Pluto trajectory and fuel constraints.[84] The search utilized large ground-based telescopes, including the Subaru Telescope on Mauna Kea and the Magellan telescopes at Las Campanas Observatory, to scan a narrow strip of sky along the spacecraft's projected path through the Kuiper Belt from 2011 to 2014.[85] These efforts discovered approximately 80 new KBOs, but none initially met the stringent geometric requirements for a feasible flyby.[85] In 2014, the Hubble Space Telescope (HST) was employed for deeper imaging in targeted fields, yielding five additional KBO discoveries, three of which were evaluated as potential targets.[86] Selection criteria focused on objects larger than approximately 40 km in diameter to ensure detectability and scientific value, with orbits allowing a safe closest approach of less than 300,000 km for high-resolution observations and a delta-V maneuver budget under 130 m/s total from the spacecraft's remaining hydrazine fuel after the Pluto encounter.[87][88] Early candidates from the ground-based search, such as the Neptune Trojan 2011 HM102 discovered in April 2011, were rejected due to their proximity to the spacecraft's path before the Pluto flyby, rendering post-Pluto targeting impossible.[71] Similarly, 2011 KU73 and other initial detections were deemed unsuitable owing to orbits outside the allowable delta-V cone or insufficient size estimates.[84] The HST observations identified promising classical KBOs, including temporary designations PT1 (2014 MU69), PT2 (2014 PN70), and PT3 (2014 OS393), but PT2 and PT3 were ultimately rejected after refined orbit determinations showed delta-V requirements exceeding 100 m/s or flyby distances too distant for optimal science return.[89][86] The primary challenge was the spacecraft's limited post-Pluto fuel, estimated at 130 m/s delta-V for targeting, which restricted the searchable sky area to a thin wedge approximately 0.01 square degrees wide extending from Pluto's position.[88] This narrow geometry, combined with the faintness of candidate KBOs (apparent magnitudes around 26-27), necessitated precise astrometry and multi-epoch observations to confirm orbits amid uncertainties in the Kuiper Belt's population density and distribution.[86] On August 28, 2015, NASA selected 2014 MU69 (later named Arrokoth) as the primary target, as it required only about 57 m/s delta-V for a close flyby at roughly 3,500 km, fitting within the fuel budget while offering a scientifically compelling cold classical KBO.[90][91] No additional KBO flybys were selected beyond Arrokoth due to the mission trajectory's geometry, which positioned the spacecraft such that subsequent targets would require delta-V maneuvers exceeding the remaining fuel after the 2019 encounter, limiting the extended mission to a single KBO observation.[88] This outcome highlighted the success of the targeted search strategy despite the challenges, enabling New Horizons to extend its scientific legacy into the outer Kuiper Belt.[85]

Arrokoth Flyby

The New Horizons mission selected Arrokoth (provisionally designated 2014 MU69) as its Kuiper Belt Object target following an extensive search process. Planning for the flyby emphasized achieving a close approach to enable high-resolution imaging and spectroscopic analysis while managing the spacecraft's limited propellant reserves. The encounter was designed to occur at a relative speed of approximately 14 km/s, with navigation relying on optical observations from the Long Range Reconnaissance Imager (LORRI) to refine the trajectory.[85] To ensure precise targeting, the mission team executed two trajectory correction maneuvers (TCMs) in 2018, incorporating data from ground-based telescopes and onboard imaging to adjust the spacecraft's path. These updates were part of the final pre-encounter navigation phase, which began in June 2018 after exiting hibernation.[16] The flyby took place on January 1, 2019, with closest approach occurring at 05:33 UTC, when New Horizons passed 3,500 km from Arrokoth's surface. This marked the most distant close encounter by any spacecraft, occurring over 4 billion miles from Earth. The encounter sequence included a series of scheduled observations spanning several days before and after closest approach, prioritizing imaging and remote sensing during the high-speed pass.[92] The primary objectives of the Arrokoth flyby were to investigate the morphology, composition, and formation mechanisms of this primitive Kuiper Belt Object, providing insights into the early solar system's planetesimal accretion processes. Initial results confirmed Arrokoth as a contact binary, consisting of two lobes gently touching at their ends, supporting models of gentle mergers in the cold classical Kuiper Belt population rather than violent collisions. This "snowman-like" structure, with the overall body measuring about 35 km in length, suggested formation from the gravitational collapse of a rotating cloud of pebbles approximately 4.5 billion years ago.[1] Key observations were captured by LORRI, achieving a resolution of 33 meters per pixel at closest approach, revealing a bilobate shape with the larger lobe (Wenu) roughly twice the size of the smaller (Wam) and both covered in relatively smooth, crater-poor terrain. Complementary data from the Ralph/Multispectral Visible Imaging Camera (MVIC) and Linear Etalon Imaging Spectral Array (LEISA) instruments indicated a uniformly red surface color, attributed to complex organic molecules such as methanol and tholins, with no detectable atmosphere, rings, or satellites. These findings highlighted Arrokoth's preservation as a "fossil" from the solar system's birth, with minimal alteration since formation.[93] During the encounter, New Horizons recorded approximately 10 GB of data across its instruments, stored onboard due to the limited downlink rate of about 1 kbps at that distance. Transmission to Earth via NASA's Deep Space Network began immediately after the flyby but proceeded slowly because of the spacecraft's increasing distance and occasional hibernations; the full dataset was not completely downlinked until October 2020.

Post-Arrokoth Observations

Following the Arrokoth flyby in January 2019, the New Horizons spacecraft continued its extended mission by conducting systematic distant observations of Kuiper Belt objects (KBOs) using the LOng Range Reconnaissance Imager (LORRI). These "KBO hunt" campaigns involved imaging dozens of distant KBOs to measure rotation light curves, phase angles, and colors, providing data on their shapes, rotational periods (ranging from 5 to 49 hours), and surface properties.[94] By 2023, the mission had completed observations of at least 31 distant KBOs, contributing to an understanding of their photometric behaviors at high phase angles not observable from Earth. Among the key targets observed in these campaigns were smaller KBOs with estimated diameters of 50–200 km, such as those in the cold classical and resonant populations. For instance, photometry of objects like 2011 HK103 and 2011 HF103 revealed low albedos (typically 0.05–0.15) and red colors consistent with organic-rich, primitive surfaces, indicating minimal alteration since the solar system's formation.[95] These measurements helped refine absolute magnitudes and sizes, with representative examples showing diameters around 100 km for hot classical KBOs like 2012 HZ84 (observed earlier but analyzed in post-flyby contexts).[96] Colors from LORRI's broadband filters suggested compositional similarities across dynamical classes, with redder hues in scattered-disk objects pointing to irradiation processes. In addition to KBO surveys, New Horizons performed ongoing heliophysics observations to probe the outer heliosphere boundaries. Instruments like the Solar Wind Around Pluto (SWAP) and Pluto Energetic Particle Spectrometer Science Investigation (PEPSSI) detected solar wind evolution, pickup ions, and energetic neutral atoms (ENAs), revealing a structured heliopause and low plasma densities beyond 45 AU.[97] These data complemented Voyager measurements, showing suprathermal ion distributions that inform models of the heliospheric sheath. Distant imaging also targeted outer solar system objects, including phase curve observations of Sedna at solar distances up to 47 AU, which yielded a Bond albedo of approximately 0.2 and confirmed its reddish spectrum indicative of complex organics. Operations during this period emphasized resource conservation, with increased hibernation durations to minimize wear on the aging spacecraft. By 2020, downlink data rates had decreased to around 100 bits per second due to the growing distance (over 50 AU), limiting observations to high-priority targets while prioritizing data return for previously collected imagery.[22] These efforts yielded insights into KBO population density, demonstrating a sparser distribution in the outer Kuiper Belt than predicted, and evolutionary trends, such as the prevalence of contact binaries and low-amplitude rotators suggesting gentle accretion histories.[98][94] As of November 2025, New Horizons continues these post-Arrokoth activities, having conducted additional distant KBO imaging and heliophysics observations while traveling beyond 60 AU from the Sun. The spacecraft entered its longest hibernation period to date on August 22, 2025, to preserve systems, with the mission extended through at least 2029 to further study the outer heliosphere and interstellar medium.[1][99]

Current Operations and Future Plans

Mission Extensions

Following the successful Pluto flyby in 2015, NASA approved the first extension of the New Horizons mission in 2016, enabling a Kuiper Belt Object (KBO) flyby and funding operations through 2021 as part of a planetary missions senior review.[100] This extension shifted the mission's focus from the Pluto system to broader Kuiper Belt exploration, including distant observations of other KBOs to study their shapes, compositions, and environments.[101] The Arrokoth phase built on this approval, with the mission specifically extended through 2021 to accommodate the January 2019 flyby of the KBO 486958 Arrokoth (provisionally known as Ultima Thule) and the subsequent downlink of collected data, which required nearly two years due to the spacecraft's distance and limited communication bandwidth.[102] This period allowed for comprehensive post-encounter analysis while continuing remote KBO surveys and heliospheric measurements.[13] In September 2023, NASA announced a further extension, committing to operate New Horizons until it exits the Kuiper Belt, projected for 2028 or 2029, following a senior review that evaluated the mission's scientific productivity and technical health.[11] The rationale emphasizes the spacecraft's unique vantage point for gathering heliophysics data on the interstellar medium and conducting wide-field surveys of distant KBOs, with annual reviews confirming ongoing viability despite increasing operational challenges like power constraints.[11][103] These extensions are supported by modest annual budgets of approximately $15 million, covering operations, data analysis, and ground support, bringing the total mission cost to over $800 million since launch in 2006.[104][17][105] The funding is primarily from NASA's Planetary Science Division, with joint contributions from the Heliophysics Division for extended observations.[11]

Recent Hibernations and Upgrades

On August 7, 2025, the New Horizons mission team successfully uploaded a major software upgrade to the spacecraft's onboard systems, enhancing its fault protection mechanisms to improve autonomous operations at greater distances from the Sun. This update, developed by engineers at the Johns Hopkins Applied Physics Laboratory, allows the spacecraft to better detect and respond to anomalies without ground intervention, extending its operational lifespan in the distant Kuiper Belt. Following the upgrade, New Horizons entered its longest hibernation period on August 22, 2025, scheduled to last until late June 2026, pending final Fiscal Year 2026 budget approval, aimed at conserving fuel and reducing wear on critical components. During this mode, the spacecraft spins stably with most systems powered down, while three instruments—SWAP, PEPSSI, and VBSDC—continue low-power measurements of charged particles and dust in the heliosphere. This approach, building on prior hibernations like the 273-day period from June 2022 to March 2023, minimizes operational costs and preserves resources for future observations. In July 2025, to mark the 10th anniversary of the Pluto flyby, NASA and the Planetary Society coordinated public outreach efforts, including a podcast interview with Principal Investigator Alan Stern highlighting mission achievements and ongoing science.[106] Concurrently, the "Progress in Understanding the Pluto System: 10 Years After Flyby" conference at the Johns Hopkins Applied Physics Laboratory featured reanalysis of New Horizons data, revealing new insights into Pluto's subsurface oceans and cryovolcanism, alongside integrations with observations from JWST and Hubble.[107] As of February 2026, New Horizons remains in its longest hibernation period, with weekly beacon signals confirming nominal engineering status and radioisotope thermoelectric generator power output at approximately 190 watts. The spacecraft is located approximately 65 AU from Earth (about 64-65 AU from the Sun) in the Kuiper Belt, traveling at roughly 14 km/s relative to the Sun, with ongoing low-rate data return from active instruments. It faces challenges from the increasing distance, including a one-way signal delay of roughly 9 hours that complicates real-time commanding and data return.[108]

Long-Term Trajectory and End of Mission

Following its flyby of Arrokoth in 2019, New Horizons continues on a heliocentric escape trajectory, having crossed Neptune's orbit on August 25, 2014, en route to the outer solar system.[109] The spacecraft's path carries it through the Kuiper Belt, with operations extended until its projected exit from this region in 2028 or 2029. Beyond the Kuiper Belt, New Horizons will venture into the outer heliosphere, potentially crossing the termination shock in the late 2020s or early 2030s.[110] The spacecraft's heliocentric velocity, currently around 14 km/s relative to the Sun, is gradually decreasing due to the Sun's gravitational influence as it recedes.[1] This hyperbolic orbit ensures New Horizons will not return to the inner solar system, instead proceeding indefinitely into interstellar space, reaching about 100 AU by the mid-2030s.[108] In its extended phase, New Horizons contributes to heliosphere science by mapping plasma interactions, magnetic fields, and dust distribution in the outer heliosphere using instruments like SWAP and PEPSSI.[97] The mission is expected to enter the interstellar medium in the 2040s, providing in-situ measurements of the local interstellar medium's properties, including neutral hydrogen and cosmic rays, to complement data from Voyager probes.[111] The end of active operations is anticipated in the mid- to late 2030s, when the radioisotope thermoelectric generator (RTG) output falls below the minimum levels required for science and communication (the RTG provided about 245 W at launch and approximately 190 W as of 2025).[112] With no propulsion for deorbiting, the spacecraft will become a silent relic drifting through interstellar space.[52] New Horizons' legacy endures through its comprehensive data archive, hosted by NASA's Planetary Data System (PDS), which includes raw and derived observations from Pluto, Arrokoth, and heliospheric measurements totaling over 6 GB.[113] This archive supports ongoing research into solar system formation and evolution, enabling analyses of primordial bodies and heliospheric boundaries by scientists worldwide.[114]

References

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