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Cyclone Gonu
Cyclone Gonu
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Super Cyclonic Storm Gonu
Gonu near peak intensity on June 4
Meteorological history
FormedJune 1, 2007
Remnant lowJune 7, 2007
DissipatedJune 8, 2007
Super cyclonic storm
3-minute sustained (IMD)
Highest winds240 km/h (150 mph)
Lowest pressure920 hPa (mbar); 27.17 inHg
Category 5-equivalent tropical cyclone
1-minute sustained (SSHWS/JTWC)
Highest winds270 km/h (165 mph)
Lowest pressure898 hPa (mbar); 26.52 inHg
Overall effects
Fatalities78 total
Missing37
Damage$4.42 billion (2007 USD)
Areas affectedWestern India, Oman, United Arab Emirates, Iran, Pakistan
IBTrACSEdit this at Wikidata

Part of the 2007 North Indian Ocean cyclone season

Super Cyclonic Storm Gonu was an extremely powerful tropical cyclone that became the strongest cyclone on record in the Arabian Sea. The second named tropical cyclone of the 2007 North Indian Ocean cyclone season, Gonu developed from a persistent area of convection in the eastern Arabian Sea on June 1, 2007. With a favorable upper-level environment and warm sea surface temperatures, it rapidly intensified to attain peak winds of 240 km/h (150 mph) on June 4, according to the India Meteorological Department. Gonu weakened after encountering dry air and cooler waters, and early on June 6, it made landfall on the easternmost tip of Oman, becoming the strongest tropical cyclone to hit the Arabian Peninsula. It then turned northward into the Gulf of Oman, and dissipated on June 7, after making landfall in southern Iran, the first cyclonic landfall in that country since 1898.

Intense tropical cyclones like Gonu are extremely rare in the Arabian Sea, and most storms in this area tend to be small and dissipate quickly.[1] The cyclone caused 50 deaths and about $4.2 billion in damage (2007 USD) in Oman, where the cyclone was considered the nation's worst natural disaster. Gonu dropped heavy rainfall near the eastern coastline, reaching up to 610 mm (24 inches), which caused flooding and heavy damage. In Iran, the cyclone caused 28 deaths and $216 million in damage (2007 USD).

Meteorological history

[edit]
Map plotting the storm's track and intensity, according to the Saffir–Simpson scale
Map key
  Tropical depression (≤38 mph, ≤62 km/h)
  Tropical storm (39–73 mph, 63–118 km/h)
  Category 1 (74–95 mph, 119–153 km/h)
  Category 2 (96–110 mph, 154–177 km/h)
  Category 3 (111–129 mph, 178–208 km/h)
  Category 4 (130–156 mph, 209–251 km/h)
  Category 5 (≥157 mph, ≥252 km/h)
  Unknown
Storm type
triangle Extratropical cyclone, remnant low, tropical disturbance, or monsoon depression

Toward the end of May 2007, the monsoon trough spawned a low-pressure area in the eastern Arabian Sea.[2] By May 31, an organized tropical disturbance was located about 645 km (400 mi) south of Mumbai, India, with cyclonic convection, or thunderstorm activity, and a well-defined mid-level circulation. The disturbance initially lacked a distinct low-level circulation; instead it consisted of strong divergence along the western end of a surface trough of low pressure.[3] A favorable upper-level environment allowed convection to improve,[4] and by late on June 1, the system developed to the extent that the India Meteorological Department (IMD) classified it as a depression.[5] It tracked westward along the southwestern periphery of a mid-level ridge over southern India. Convection continued to organize, and early on June 2, the Joint Typhoon Warning Center (JTWC) classified the storm as Tropical Cyclone 02A, about 685 km (425 mi) southwest of Mumbai.[6]

Upon first forming, the system contended with the entrainment of dry air to the northwest of the storm, which was expected to limit intensification.[6] The storm steadily intensified, and early on June 2 the IMD upgraded it to deep depression status.[7] Later in the day the IMD classified the system as Cyclonic Storm Gonu about 760 km (470 mi) southwest of Mumbai, India.[8] As a mid-latitude trough developed over Pakistan, Gonu turned to the north and northeast,[9] though it resumed a westward track after ridging built to the north of the storm.[10] With a solid area of intense convection, it rapidly intensified to attain severe cyclonic status early on June 3,[11] and with good outflow the JTWC upgraded it to the equivalent of a minimal hurricane.[12] The dry air ultimately had a smaller impact on the intensification than previously estimated. A well-defined eye developed in the center of convection, and after moving over a local increase in ocean heat content, Gonu rapidly deepened.[13]

Cyclone Gonu off the coast of Oman on June 5

Late on June 3, the IMD upgraded the storm to Very Severe Cyclonic Storm Gonu.[14] With warm waters,[15] low amounts of vertical wind shear, and favorable upper-level outflow, Gonu strengthened further to attain peak 1-min sustained winds of 270 km/h (170 mph)[16] and gusts to 315 km/h (195 mph), about 285 km (175 mi) east-southeast of Masirah Island on the coast of Oman.[17] The IMD upgraded it to Super Cyclonic Storm Gonu late on June 4, with peak 3-min sustained winds reaching 240 km/h (150 mph) and an estimated pressure of 920 mbar.[18] This made it the first super cyclonic storm in the Arabian Sea on record.[15]

After the storm maintained peak winds for about six hours, the IMD downgraded Gonu to very severe cyclonic storm status late on June 4.[2] Gonu's eye became cloud-filled and ragged, and the cyclone gradually weakened due to cooler water temperatures and drier air as it approached the Arabian Peninsula.[19] Due to land interaction with Oman, the inner core of deep convection rapidly weakened, and over a period of 24 hours the intensity decreased by 95 km/h (60 mph).[20] According to the IMD, Cyclone Gonu crossed the easternmost tip of Oman near Muscat early on June 6, with winds of 143 km/h (89 mph).[2] Although the winds continued to gradually decrease, overall organization increased slightly in the hours prior to landfall; Gonu maintained a well-defined low-level structure with a weak eye.[21]

After emerging into the Gulf of Oman, the cyclone briefly re-intensified slightly,[22] possibly due to the warm waters.[15] However, increasing wind shear and entrainment of dry air from the Arabian Peninsula continued to remove deep convection from its eastern semicircle.[23] On June 6, the cyclone turned to the north-northwest,[24] and later that day the JTWC downgraded Gonu to tropical storm status.[25] The IMD followed suit by downgrading Gonu to severe cyclonic storm status, and later to cyclonic storm status early on June 7.[26][27] Gonu crossed the Makran coast in Iran six hours later, and the IMD stopped issuing advisories on the cyclone.[28] This made it the first tropical cyclone on record to hit the country since 1898. After landfall, Gonu persisted as a remnant low over Iran through June 8.[15]

Preparations

[edit]

The Oman Chairman of the National Committee for Civil Defence, General Malek Bin Sulaiman Al Ma'amari, remarked the nation had already developed a contingency plan, which included the activation of army and police personnel after the storm's passage. Significant damage was expected, especially in northeastern areas, along with up to 150 mm (6 in) of rainfall and very strong winds.[29] Officials recommended citizens evacuate from potentially affected areas,[30] and about 7,000 people were forced to leave Masirah Island due to the threat of high surf and strong winds.[31] Overall, more than 20,000 people evacuated to emergency shelters.[32] A state of emergency was declared for the nation.[30] The Omani national weather service warned that the cyclone was expected to be worse than the destructive cyclone that hit Masirah Island in 1977.[33] The Mina al Fahal oil terminal closed for over three days due to the threat of the storm.[34] Omani officials closed government offices for two days and declared a five-day-long national holiday. Most businesses near the coastline were closed prior to the announcement.[35] The nation's Civil Aviation Authority, along with Muscat International Airport (then named as "Seeb International Airport") and Salalah International Airport canceled all flights at 20:00 UTC on June 5.[36]

Map showing rainfall totals around the Gulf of Oman between May 31 and June 7, 2007. The red areas show where rainfall exceeded 200 mm (8 inches).

In Saudi Arabia and the United Arab Emirates, both members of OPEC, no official warnings had been issued due to Gonu. The storm was not expected to disrupt oil supplies from these two nations.[30] However, oil prices rose early on June 5 because of concerns of disruptions caused by Gonu, as well as the threat of nationwide strikes in Nigeria, Africa's biggest oil producer. Crude oil for July delivery rose $1.13, or 1.7 percent, to $66.21 Monday on the New York Mercantile Exchange, the highest close in 15 days. Futures reached $66.48, the highest intraday price since April 30. The contract was at $65.95 a barrel, down 26 cents, in after-hours electronic trading at 9:43 a.m. Tuesday in Singapore.[37] Tom Kloza, chief oil analyst at the Oil Price Information Service, said he doubted the increase could be attributed to Gonu. "I don't know if you can really attribute any of the gain to the cyclone", he said. "It's an excuse, as opposed to a reason, for the rise in prices."[38]

In Pakistan, officials recommended fishermen remain within 50 km (30 mi) of the coastline, due to anticipated rough waves in the open ocean.[39] Naval authorities in the United States warned ships to avoid the cyclone in the Arabian Sea.[40]

The Iran Department of Meteorology declared storm warnings for the country's southeastern coastline; the agency anticipated moderate to severe precipitation and gusty winds.[41] Prior to the arrival of the cyclone, about 40,000 people,[42] including around 4,000 students at the International University of Chabahar,[43] evacuated coastal areas of the country to at least 1 km (0.6 mi) inland.[42] All flights in and out of the Konarak Airport were canceled during a 48-hour period. Additionally, all hospitals in Sistan and Baluchestan Province were put on red alert.[43] The Iran chapter of the Red Cross advanced the delivery of necessary relief supplies.[44]

Impact

[edit]
Road damage in Muscat, Oman

Across its path, Cyclone Gonu caused heavy damage and many fatalities.[2] About seven hours before passing near the northeastern Oman coastline, Gonu began affecting the country with rough winds and heavy precipitation; rainfall totals reached 610 mm (24 in) near the coast.[45][46] Gonu produced strong waves along much of the coastline,[45] leaving many coastal roads flooded.[41] There was a 5.1 meter (17 foot) storm surge and a 200 m (660 ft) incursion of seawater inland at Ras al-Hadd; other areas along the coast had similar levels.[47]

Oman

[edit]

Strong winds knocked out power and telephone lines across the eastern region of the country, leaving thousands isolated until the lines were repaired hours later. The cyclone caused extensive damage along the coastline, including in the city of Sur and the village of Ras al Hadd at the easternmost point of the Omani mainland.[48] In Muscat, winds reached 100 km/h (60 mph), leaving the capital city without power. Strong waves and heavy rainfall flooded streets and some buildings. Police workers in the city sent text messages to keep people away from flooded streets to prevent electrocutions. Little damage was reported to the oil fields of the nation.[32] The liquefied natural gas terminal in Sur, which handles 10 million tonnes of gas each year, was badly hit by the storm and could not be operated.[49] Overall, the cyclone killed 50 people in the country; by the fourth day after it struck the country, 27 people had been reported missing.[2] Around 20,000 people were affected,[50] and damage in the country was estimated at $4.2 billion (2007 USD).[2]

United Arab Emirates

[edit]
Costliest known North Indian cyclones (adjusted for inflation)
Rank Cyclone Season Damage
(2025 USD)
1  ESCS  Nargis 2008 $22.9 billion
2  CS  Senyar 2025 $20.1 billion
3  SuCS  Amphan 2020 $19.3 billion
4  ESCS  Fani 2019 $10.2 billion
5  SuCS  BOB 06 1999 $8.58 billion
6  SuCS  Gonu 2007 $6.86 billion
7  ESCS  ARB 02 1998 $5.93 billion
8  ESCS  Phailin 2013 $5.89 billion
9  ESCS  Hudhud 2014 $4.87 billion
10  VSCS  Vardah 2016 $4.53 billion

Fierce waves pushed large amounts of water to coastal areas in Fujairah of the United Arab Emirates, forcing roads to be closed and traffic diverted. Civil defence and police were on duty to manage the road closures, while municipal workers pumped the excess water off the roads. The road connecting Kalba and Fujairah was closed due to the road being submerged by water.[51] The waves along the coastline were reported to be 10 m (32 ft) high, which destroyed about a dozen fishing boats. About 300 boats were moved from the water or emptied of equipment,[52] and overall damage to the port of Fujairah was reported as severe. A boat sank by the port, leaving its ten passengers missing.[53]

Iran

[edit]

Upon striking Iran, Gonu dropped moderate to heavy rainfall, including 74 mm (2.91 in) in the city of Chabahar.[42] Winds reached 111 km/h (69 mph),[32] which caused power outages and damaged some homes made of clay;[42] the power outage led to some fires across the city. The rainfall flooded at least 40 houses,[43] and resulted in the temporary closure of several major roads.[32] Gonu produced a storm tide of 2 m (6.5 ft) in some locations,[54] with many homes near the coastline receiving damage.[34] In Jask, heavy rainfall overflowed a river, killing three people in a vehicle caught in the water.[55] Flooding from the rainfall also destroyed a dam in Nikshahr County.[54] Throughout the country, the cyclone caused 28 deaths,[2] including 20 from drowning; damage in Iran was estimated at 2 billion (2007 IRR, $216 million 2007 USD).[54]

Pakistan

[edit]

Gonu caused strong gusty winds and torrential rainfall along Pakistan's Arabian Sea coast from Karachi to Gwadar.[56] The cyclone was reported to have sunk a number of boats off the eastern coast of Gwadar.[57] It was feared that fishing launches that had ventured into the open sea may have been stranded. At least three houses and one school were destroyed and 210 anchored fishing boats were badly damaged anchored in the coastal town of Sar Bandar in Baluchistan province[58]

Aftermath

[edit]
Flipped car and flooding on a street in Muscat, Oman
Satellite animation showing the life cycle of Gonu

Flights to and from Muscat resumed after three days while Fujairah reopened on June 7 after it was closed the day before.[49] The cyclone caused little impact to oil facilities along its path; after the initial price rises, oil dropped over US$2 per barrel as a result.[59] Across the northern Arabian Sea, the passage of Gonu produced stronger winds and significant upwelling – an oceanographic phenomenon that involves the replacement of the nutrient-depleted surface water with deeper nutrient-rich water; the passage caused a significant increase in phytoplankton.[60] Additionally, the cyclone delayed the arrival of the Indian Ocean south-west monsoon in the Western Ghats in India.[61]

In Oman, production of desalinated water was interrupted, as both of Oman's desalination plants failed. The first, Ghubrah, lost supplies of natural gas, halting production; while the second, Barka, sustained a damaged switchgear due to flooding. These plants provided water to Muscat's 631,000 residents and surrounding areas, triggering severe water shortages across eastern Oman. To rectify the situation, officials used water tanks. The water returned to near normal in five days, as the two plants returned to service. Additionally, electricians worked quickly to repair the power outages across the region.[62] Five days after Gonu hit, utilities were restored to most of Muscat and the coastal provinces. The Omani army assisted residents in returning to their houses. Even though the Omani government did not request any international aid, the United States offered assistance through naval ships in the area; this was eventually rejected.[46] The country lost an estimated $200 million (2007 USD) in oil exports.[63] In the months after the storm, the government allocated funds for the removal of debris and trees, as well as restoration of roads in tourist areas.[64] Additionally, the National Committee for Civil Defence set up 139 buildings to provide temporary housing for 8,192 people. Services such as water and electricity were gradually restored, and people returned to their homes. By two weeks after the storm's passage, most of those remaining in shelters were from Qurayat, one of the most severely affected villages.[65]

After the passage of the cyclone, the Iran chapter of the Red Cross and its volunteers worked in conjunction with the military to distribute relief supplies to villages using trucks and helicopters. The branch in Sistan and Baluchestan Province distributed over 10,000 blankets, 1,300 tents, 400 clothing items, 82,000 loaves of bread, and 87,000 bottles of water to affected citizens.[44] In total, 61,558 families received aid from the Red Cross in Iran.[66] The Iranian government provided monetary relief to the affected people. Officials worked to restore roads, bridges, and power systems in the affected areas, although repairs were more difficult in some locations; by a week after the storm, several villages remained surrounded by floodwaters.[67]

Records

[edit]

Cyclone Gonu set several intensity records. When it became a very severe cyclonic storm on June 3, Gonu became the strongest tropical cyclone on record in the Arabian Sea.[14][68] It was the only super cyclonic storm, which is a tropical cyclone with 3-minute sustained winds of at least 220 km/h (135 mph), in the region, until Cyclone Kyarr 12 years later.[2] The JTWC estimated peak 1-minute sustained winds of 270 km/h (170 mph), the highest 1-minute sustained winds of any cyclone in the North Indian Ocean until Cyclone Fani 12 years later.[16] On June 6, Gonu made landfall in extreme eastern Oman with winds of 150 km/h (95 mph),[2] making it the strongest tropical cyclone on record to strike the Arabian Peninsula.[69] With a damage total of $4.2 billion (2007 USD) and 50 deaths,[2] Gonu became the worst natural disaster on record in Oman.[68] Additionally, the storm was only the second cyclonic storm on record to strike Iran, with the other one doing so on June 4, 1898.[2]

See also

[edit]

References

[edit]
[edit]
Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Cyclone Gonu was a super cyclonic storm that formed over the east-central on June 1, 2007, and became the strongest on record in the northern , reaching Category 5-equivalent intensity with maximum sustained winds of 127 knots (235 km/h) and a minimum central pressure of 920 hPa. It tracked north-northwestward, making landfall near , , on June 6 as a very severe cyclonic storm with winds of 140 km/h, before weakening and striking southeastern on June 7. The cyclone's was fueled by warm sea surface temperatures exceeding 30°C and high atmospheric moisture, though it dissipated quickly over land due to increasing and cooler waters. Gonu's impacts were devastating across the affected regions, particularly in Oman, where it caused 49 deaths and left 27 people missing, while displacing around 20,000 residents and inflicting approximately $4 billion in damages to infrastructure, including roads, water supplies, and coastal facilities. Heavy rainfall, peaking at 943 mm in some areas of Oman, triggered widespread flooding and landslides, exacerbating the destruction in a region unaccustomed to such intense cyclones. In Iran, the storm resulted in 20 to 23 fatalities, $216 million in economic losses, and flooding from 74 mm of rain combined with a 2-meter storm surge that inundated homes and roads. The United Arab Emirates experienced minor effects, including 10 missing persons from a boat incident at Fujairah port. Meteorologically, Gonu marked the first super cyclone in the since reliable records began, highlighting vulnerabilities in forecasting for the area due to limited coverage along Oman's coast and challenges in models. Its oceanic influence included significant cooling of sea surface temperatures by 1.7–6.5°C and deepening of the to up to 140 meters in the , demonstrating the cyclone's power in altering regional marine conditions. The event prompted evacuations in southeastern and a multi-day in from June 5 to 9, underscoring the rarity of such storms in the region. Overall, Gonu caused approximately 70 deaths (with dozens missing) and over $4 billion in damages, serving as a critical for in the .

Naming and background

Naming origin

The naming of tropical cyclones in the North Indian Ocean basin, encompassing the and , is managed by the (IMD) as the Regional Specialized Meteorological Center (RSMC) designated by the (WMO). Under this system, established in 2004, cyclones reaching cyclonic storm intensity (winds of at least 48 km/h) are assigned names sequentially from a pre-approved list contributed by member countries of the WMO/ESCAP Panel on Tropical Cyclones. These names are selected to be short, neutral, and culturally significant, with each of the participating nations—initially eight, including the —providing eight names to ensure equitable representation and avoid repetition once used. The name "Gonu" was contributed by the Maldives to this panel's list. In Dhivehi, the Maldivian language, "Gonu" refers to a traditional woven from palm leaves, reflecting local cultural elements in line with the naming guidelines that prioritize non-offensive, pronounceable terms meaningful to the contributing country. Cyclone Gonu was the second named of the 2007 North Indian Ocean cyclone season, following Cyclonic Storm Akash in May. The IMD assigned the name upon Gonu's classification as a cyclonic on June 2, 2007, adhering to the sequential order from the .

2007 North Indian Ocean cyclone season

The 2007 North Indian Ocean cyclone season exhibited above-average activity in terms of total disturbances, with 12 cyclonic disturbances forming across the and , compared to the 1965–2023 climatological average of 11.2 such systems per year. Of these, four reached cyclonic intensity and received names from the : Akash, Gonu, Yemyin, and Sidr, which was below the typical annual average of about five named storms. Two systems intensified significantly, with Gonu classified as a super cyclonic and Sidr as a very severe cyclonic , contributing to the season's elevated overall energy despite the lower number of named storms. This heightened activity was attributed to anomalously warm sea surface temperatures exceeding 28–30°C in key formation regions, providing favorable conditions for development. The season began with Cyclonic Storm Akash forming in the during mid-May, followed by Gonu as the second named storm in early . These early events highlighted an active pre- phase, with additional depressions forming in the . Later, Yemyin and Sidr emerged during the monsoon and post-monsoon periods, respectively, underscoring the basin's bimodal activity pattern. Contributing environmental factors included ENSO-neutral conditions prevailing through much of the year, which avoided the suppressive effects of strong El Niño events on cyclone genesis. A positive phase of the also played a role, characterized by warmer sea surface temperatures in the western —including the —enhancing and moisture availability for formation. These conditions, combined with low vertical , supported the season's robust activity relative to the 1971–2000 baseline average of approximately 5.5 systems reaching cyclonic storm intensity.

Meteorological history

Formation and initial development

A persistent area of convection in the eastern was first tracked by the (IMD) in late May 2007. This disturbance organized into a over the east-central on 31 May 2007, coinciding with the onset phase of the southwest . The concentrated into a depression on 1 2007. At 12:00 UTC on 1 June 2007, the IMD upgraded it to cyclonic storm status, naming it Gonu as the second named of the 2007 North Indian Ocean cyclone season, with the center located at 15.0°N 68.0°E, sustained winds of 45 knots (83 km/h), and an estimated central pressure of 992 hPa. Initial organization benefited from favorable environmental conditions, including low vertical of approximately 10 knots and sea surface temperatures exceeding 26.5°C. Under steering influences from a subtropical to the north, the tracked initially north-northwestward at 5–10 km/h.

Intensification and peak intensity

Following its initial development, Cyclone Gonu underwent steady intensification. By 0300 UTC on June 3, it had strengthened into a severe cyclonic , with sustained winds increasing to around 65 knots (120 km/h) based on 3-minute averages. The system continued to organize, featuring a well-defined eye visible on by 0000 UTC on June 4, surrounded by intense with cloud-top temperatures near -70°C. Rapid intensification commenced around 1800 UTC on June 3, driven by sea surface temperatures exceeding 30°C in the central and initially low vertical of about 10 knots, which supported enhanced and outflow. The IMD upgraded Gonu to very severe cyclonic status at 1800 UTC on June 3, with winds reaching 105 knots (195 km/h). This phase saw the 's structure evolve into a more symmetrical form, with the eye maintaining clarity amid deepening . Gonu achieved its peak intensity at 1500 UTC on June 4, classified as a super cyclonic storm by the IMD, with maximum 3-minute sustained of 127 knots (235 km/h) and a minimum central of 920 hPa. Concurrently, the (JTWC) estimated 1-minute sustained of 145 knots (270 km/h) and a central of 914 hPa, equivalent to a Category 5 hurricane on the Saffir-Simpson scale. Despite vertical rising to 20-30 knots during this period, the 's intensity peaked briefly for about 6 hours, facilitated by the warm oceanic environment and a distinct eye feature. The IMD noted a rapid T-number increase of 3.0 over 24 hours leading to this maximum, marking Gonu as the strongest recorded in the at the time.

Landfall and dissipation

After attaining peak intensity, Cyclone Gonu shifted its track to the north-northeast on June 5, 2007, steered by a mid-level trough that enhanced divergence aloft and promoted continued organization despite increasing . The cyclone made its first on June 6, 2007, near in , with maximum sustained winds of 77 knots (143 km/h; 3-minute average), equivalent to approximately Category 1 on the Saffir–Simpson hurricane wind scale (1-minute sustained winds). This marked the strongest on record in the , with the center crossing the northeast coast between 0200 and 0300 UTC at approximately 22.5°N, 59.5°E. Following , Gonu emerged into the , where cooler sea surface temperatures and land interaction caused rapid weakening to a severe cyclonic storm with winds decreasing to around 102 km/h (55 knots) by late June 6. The system continued north-northwestward under the influence of the same mid-level trough, maintaining a broad circulation as it approached the Iranian coast. On June 7, 2007, Gonu made a second landfall on Iran's coast near 25.5°N, 58.5°E as a tropical storm with maximum sustained winds of 85 km/h (45 knots), crossing between 0300 and 0400 UTC. Over land, the cyclone continued to weaken due to frictional effects and from the terrain. By June 8, 2007, Gonu had dissipated into a remnant over , centered near 27°N, 60°E, with no further tropical development possible.

Preparations

In Oman

Omani authorities began issuing cyclone warnings through the on June 3, 2007, mobilizing the country's emergency response apparatus in anticipation of the storm's approach. These alerts escalated on June 5, when a was declared, particularly on , the first area expected to be impacted. Warnings were disseminated via text messages urging residents to avoid low-lying coastal zones, while similar alerts were issued in neighboring and . In response to the threat, over 20,000 residents were evacuated from vulnerable coastal areas, with a focus on and surrounding governorates, including the complete evacuation of two islands and 11,000 workers from ports such as and Qabus. To facilitate these efforts, authorities closed schools across affected regions, repurposing them as safe havens equipped with food, bedding, and essential supplies; Seeb International Airport suspended all flights, and seaports including halted operations while oil exports were paused by preventing tanker departures. Additionally, 12 emergency shelters were activated, and the along with public and private institutions shut down until the immediate danger passed. Preparations also involved the deployment of over 4,000 trained personnel, alongside and military troops, particularly on to support shelter operations and medical services. Authorities stockpiled food, water, medicine, and other supplies in government-provided dwellings and shelters to ensure readiness for those displaced.

In Iran

As Cyclone Gonu tracked into the , Iran's Meteorological Organization issued storm warnings on June 5, 2007, targeting along the southeastern coast, alerting residents to prepare for heavy rains, high waves, and potential flooding. These warnings were disseminated through radio and television broadcasts, urging evacuations from coastlines and riverine areas prone to overflow. In response, authorities evacuated approximately 40,000 people from low-lying coastal villages near the border to safer, elevated locations, including relocations in and surrounding areas. In the port city of , hundreds of residents within 1 kilometer of the shoreline were moved, along with staff from Imam Ali Hospital to inland safe zones. The Iranian Red Crescent Society (IRCS) played a central role in coordination, mobilizing 528 relief workers, 43 staff members, two helicopters, motor pumps, ambulances, and emergency stocks such as 22,000 cans of tuna, 2,000 blankets, and 130 tents for distribution. Preparations also included helicopter drops of supplies to at-risk villages and the establishment of emergency shelters in collaboration with government task forces, with a focus on mitigating flash flooding in regions across and Baluchestan. The IRCS held urgent meetings with provincial ministries to align resources, placing hospitals on high alert and prepositioning medicines and . Similar precautionary alerts were issued in neighboring , though the primary emphasis remained on southeastern coastal threats.

In other countries

In the , the National Center of Meteorology issued high sea warnings on June 5, 2007, advising vessels to avoid the due to expected strong winds and high tides up to 10 feet along the Fujairah coast. No large-scale evacuations were conducted, though marine activities were restricted in coastal areas and an emergency was established to monitor potential effects. In , the issued advisories on June 6, 2007, urging fishermen to remain ashore and avoid venturing into the , particularly along the coasts of and , where rough seas were anticipated. India's preparations were minimal, with brief alerts issued in on June 3, 2007, instructing district collectors in coastal areas to remain vigilant for potential swell effects from the cyclone. No evacuations occurred, but authorities monitored conditions closely, advising fishermen to avoid the waters for 24 hours due to unpredictable weather patterns.

Impact

Oman

Cyclone Gonu made landfall near Sur on 's eastern coast on June 6, 2007, as a very severe cyclonic storm, unleashing extreme rainfall of up to 610 mm in the Sur area, which triggered widespread flooding and landslides across the region. The storm also generated a peaking at approximately 5 meters at Ras al-Hadd, the eastern tip of the , inundating coastal areas up to 200 meters inland and exacerbating flood damage along 270 kilometers of shoreline. These meteorological effects led to the destruction of homes and key , including the Al-Ghubrah power and desalination plant near , which lost supplies and sustained damage from flooding, interrupting potable water production for the capital area. The cyclone resulted in 49 confirmed fatalities and 27 people missing in , with most deaths attributed to in flash floods and collapses of structures overwhelmed by the deluge. Over 20,000 individuals were left homeless due to the destruction of residences in coastal and low-lying areas, particularly around and Sur. Preparatory evacuations of tens of thousands from vulnerable zones helped limit the overall casualty toll. Economic losses from Gonu in totaled approximately $4 billion (2007 USD), marking it as the country's costliest on record, driven by damage to housing, transportation networks, and utilities. suffered significantly, with flooding destroying thousands of date palm trees—a staple —across affected farms and disrupting systems in the fertile eastern regions.

United Arab Emirates

Although Cyclone Gonu did not make direct landfall in the , its powerful swells generated high waves along the eastern coastline, reaching up to 10 meters in height and causing significant disruptions to maritime activities. A boat sank near the due to these waves, leaving 10 passengers reported missing at sea. Ports in Fujairah and sustained damage, including impacts to oil terminals and fishing harbors, where about a dozen fishing boats were destroyed and around 300 others were relocated or emptied to prevent further losses. The Fujairah port was temporarily closed but reopened on June 7, 2007, while maritime traffic faced broader disruptions in the , with several vessels grounded amid the rough seas. In addition to wave-related impacts, the cyclone brought heavy rainfall leading to urban flooding in Dubai and Sharjah. Streets in Sharjah, particularly in areas like Kalba, were inundated, though floodwaters receded by June 8, 2007, with no reported deaths. Coastal infrastructure, including sandbag barriers, was breached by tidal surges, affecting homes and roads in Fujairah and nearby regions, with overall damage estimated in the tens of millions of USD.

Iran

Cyclone Gonu made a second in on June 7, 2007, primarily impacting the provinces of and Baluchestan, Hormozgan, and parts of . The storm generated intense rainfall, with accumulations reaching up to 74 mm in areas like , accompanied by a 2-meter storm tide that triggered river overflows and extensive flash flooding across coastal and inland regions. These conditions led to widespread inundation of agricultural lands, affecting approximately 5,000 hectares of farmland and causing substantial losses to crops and livestock in the arid southern terrain. The flash floods and structural failures from the deluge resulted in 23 fatalities across the affected provinces, mainly due to in floodwaters and collapses of vulnerable buildings constructed from local materials like clay and mud bricks. Infrastructure suffered severe damage, including the destruction of around 1,200 homes, numerous roads, and bridges, which isolated villages and hindered emergency response efforts in remote areas. Overall economic losses in totaled $216 million (2007 USD), encompassing repairs to housing, transportation networks, and agricultural recovery. Power outages disrupted service to about 50,000 households for several days, leaving communities without amid ongoing flooding and complicating access to clean water and communications. Prior warnings from meteorological authorities enabled limited evacuations along the coast, helping to reduce the potential death toll.

Pakistan

Cyclone Gonu produced distant effects in , primarily impacting coastal areas of province through strong winds, rough seas, and associated heavy rainfall. Winds reaching up to 60 km/h battered the coastline, damaging over 100 fishing boats anchored in and approximately 100 more in , while rough seas contributed to the destruction of around 30 additional boats in the Sur Bandar area near . Several homes were also affected, including 40 houses washed away in Sur Bandar and partial damage to at least one private residence inland in . Heavy rainfall triggered minor flooding in , which inundated local roads and partially damaged a building, exacerbating disruptions to daily activities in fishing communities. No fatalities were reported in from these effects. Economic losses centered on the fisheries sector, severely impacting livelihoods for local fishermen whose boats formed the backbone of coastal trade; the Balochistan government subsequently announced compensation for the damaged vessels. Advisories from the urged fishermen in Gwadar, Jiwani, and surrounding areas to remain ashore for 24 hours amid the rough conditions, leading to temporary halts in maritime activities.

Aftermath

Humanitarian response

In the immediate aftermath of Cyclone Gonu, Oman declared a and mobilized national resources for rescue and relief operations. Over 4,000 trained personnel were deployed to affected areas, alongside troops and police forces tasked with providing shelter, medical services, and search efforts for those trapped in flooded homes. More than 20,000 people were evacuated to government shelters equipped with food, bedding, and medicine, while schools were converted into safe havens. These efforts focused on the hardest-hit regions around and , where the cyclone caused 49 deaths and 27 missing, displacing around 20,000 residents. Oman declined offers of international assistance from Gulf Cooperation Council countries and organizations like , stating that national capacities were sufficient to handle the crisis. In neighboring , the government and the Iranian Red Crescent Society (IRCS) launched rapid response operations in Sistan-Baluchistan and Hormozgan provinces, where the storm's remnants triggered flooding and stranded villagers. IRCS teams, supported by 528 relief workers and 43 staff, distributed essential supplies including 22,000 cans of , 10,000 kg of , 2,000 blankets, and 130 tents to affected communities, while helicopters conducted 46 flights to deliver aid to remote areas. A temporary medical camp was established by local hospital staff, and provincial task forces repaired like roads and power lines. These actions aided approximately 7,918 families in Sistan-Baluchistan alone and rescued residents from flooded villages, contributing to a total of 23 deaths reported in . The expressed readiness to support with logistical aid, though specific deployments of medical teams or helicopters were not activated due to Oman's self-sufficiency. Overall, the humanitarian response emphasized coordinated national efforts, with international organizations like the UN Office for the Coordination of Humanitarian Affairs (OCHA) monitoring the situation but not mobilizing major funds, as no formal appeals were issued.

Reconstruction and recovery

Following Cyclone Gonu, the Omani government launched extensive reconstruction initiatives, with estimated costs for repairs exceeding $1 billion. Power and services were restored to most areas of and coastal provinces within six days of the cyclone's on June 6, 2007, while water supplies were similarly reestablished through emergency measures. The critical Ghubrah desalination plant, which supplies much of the capital's potable water, recovered to 90% capacity by June 12, achieving full operational levels in the ensuing months. Additionally, Sultan Qaboos bin Said allocated 7 million Omani riyals (approximately $18 million) for victim support, complemented by an 81 million Omani riyal from the Arab Fund for new developments, including fishing harbors, pipelines, and educational facilities. Economic recovery in faced challenges from ripple effects, including over $200 million in lost export revenues due to a two-day halt in production at key facilities. providers, benefiting from Oman's relatively high coverage rates, anticipated substantial payouts to offset , though assessments were delayed by widespread flooding and . In the longer term, the prompted policy enhancements for resilience, such as dam construction, road network restructuring, and heightened public awareness campaigns to mitigate future risks. In , where the cyclone struck on June 7, 2007, the government allocated resources equivalent to roughly half the estimated $216 million in total damages for repairing roads, homes, and utilities, with 80% of , , and telecommunications infrastructure restored within three days. Over 20,000 homes were flooded, affecting 560,000 people, and repair efforts prioritized reconnecting isolated villages, achieving approximately 80% completion of major road and residential reconstructions by the end of 2007. These initiatives built on initial distributions, focusing on medium-term economic stabilization in the shrimp-farming and agricultural sectors.

Environmental effects

Cyclone Gonu induced notable ecological changes in the through vertical mixing and , which brought nutrient-rich subsurface waters to the surface and triggered blooms shortly after the storm's passage. Satellite data revealed two distinct blooms: one northeast of with chlorophyll-a concentrations up to 3.5 mg m⁻³ and another in the eastern central reaching 0.4 mg m⁻³, representing a tenfold increase over pre-storm levels of 0.05–0.2 mg m⁻³. This nutrient injection enhanced primary biological productivity at the base of the marine , temporarily benefiting higher trophic levels such as by increasing available food resources. The cyclone's intense winds and associated cooling of sea surface temperatures, which dropped below 28.5°C in its wake, disrupted regional atmospheric patterns and contributed to a delay in the Indian southwest 's advancement. Despite an early onset over on May 28, 2007, the storm's presence halted further progression into central and until June 7, 2007. This altered the typical timing of seasonal rainfall and potentially influenced longer-term climatic variability in the region. Along Oman's coastline, the storm surge—peaking at over 5 meters at Ras al Hadd—drove severe erosion and habitat degradation, particularly affecting sensitive ecosystems like mangroves and coral reefs. High waves and sediment-laden surge caused mechanical breakage, dislodgement, and smothering of corals in shallow waters (<8 m depth) from Muscat to the UAE border, leading to substantial losses in live cover and biodiversity. Mangrove stands, vital for coastal protection, also suffered damage from the surge and flooding, exacerbating vulnerability in urban-proximate areas.

Records

Intensity records

Cyclone Gonu set several intensity records for tropical cyclones in the , marking it as an exceptionally powerful storm for the basin. According to the (IMD), the cyclone reached a minimum central of 920 hPa on June 4, 2007, which was the lowest on record for the at the time. The (JTWC) estimated an even lower central of 914 hPa, further underscoring the storm's extreme depth. This surpassed previous benchmarks in the region, including the 1998 Gujarat cyclone's 958 hPa by 38 hPa, establishing Gonu as the most intense cyclone documented in the North Indian Ocean's branch prior to later events like Cyclone Kyarr in 2019. In terms of wind speeds, Gonu achieved peak 3-minute sustained winds of 127 knots (235 km/h) as assessed by the IMD, classifying it as the first super cyclonic storm ever recorded in the Arabian Sea. The JTWC reported higher 1-minute sustained winds of 145 knots (270 km/h), equivalent to a Category 5 hurricane on the Saffir-Simpson scale and the strongest winds observed in the basin up to that point. These speeds exceeded prior records, such as the 1998 Gujarat cyclone's estimated 90 knots (165 km/h) by approximately 40 knots (75 km/h), highlighting Gonu's unprecedented ferocity compared to earlier Arabian Sea systems. The storm's intensity made it the strongest tropical cyclone to impact the Arabian Peninsula on record. Gonu also demonstrated remarkable , with the IMD noting a increase of about 65 km/h over 24 hours from to , 2007, as the evolved from a very severe cyclonic to super cyclonic status. This rate was exceptional for the , where such explosive development is rare due to typically unfavorable environmental conditions like and cooler sea surface temperatures. The JTWC observed an even more dramatic 24-hour gain of 75 knots (139 km/h) during the same period, from 70 knots to 145 knots, further emphasizing the 's record-breaking acceleration. These metrics not only broke basin-specific thresholds but also contributed to Gonu's overall legacy as a benchmark for extreme behavior in the region.

Societal impact records

Cyclone Gonu stands as the worst in Oman's modern , inflicting approximately $4 billion (2007 USD) in damages that surpassed the local effects of the 2004 in the region. The storm's exceptional intensity as the first super cyclone to strike the amplified its destructive reach, causing widespread flooding and infrastructure collapse along Oman's eastern coast. In , Gonu resulted in 50 fatalities, marking the highest death toll from any cyclone in the country's . This surpassed previous tropical systems, with the majority of deaths occurring due to in flash floods and structural failures in coastal areas like and Sur. For , Gonu represented only the second cyclone to make since 1898, with 23 deaths that established the highest toll from a tropical system in the nation's . The storm's remnants triggered severe flooding in southern provinces such as Hormozgan and Sistan-Baluchestan, overwhelming unprepared communities and agricultural zones. Regionally, Gonu caused 78 to 100 fatalities across , , and adjacent areas, alongside at least 37 missing persons, setting a grim benchmark for cyclones in terms of human cost. These figures underscore the cyclone's role in highlighting vulnerabilities in the Arabian Peninsula's disaster preparedness.

References

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