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The 60th parallel north is a circle of latitude that is 60 degrees north of Earth's equator. It crosses Europe, Asia, the Pacific Ocean, North America, and the Atlantic Ocean.

Although it lies approximately twice as far away from the Equator as from the North Pole, the 60th parallel is half as long as the Equator line, due to the cosine of 60 degrees being 0.5. This is where the Earth bulges halfway as much as on the Equator.

At this latitude, the Sun is visible for 6 hours, 7 minutes during the June solstice and 5 hours, 52 minutes during the December solstice.[1] The maximum altitude of the Sun is 53.44° on 21 June and 6.56° on 21 December. The maximum altitude of the Sun is > 15.00º in October and > 8.00º in November.[2]

The lowest latitude where white nights can be observed is approximately on this parallel. White nights in the 60th parallel north occur around the June Solstice (Summer Solstice in the Northern Hemisphere).

During the summer solstice, nighttime does not get beyond nautical twilight, a condition which lasts throughout the month of June. It is possible to view both astronomical dawn and dusk every day between August 22 and April 21.

Around the world

[edit]

Malachy Tallack wrote a book, Sixty Degrees North: Around the World in Search of Home, about his travels along the general line of the parallel, starting and finishing at Shetland.[3][4]

Starting at the Prime Meridian and heading eastwards, the parallel 60° north passes through:

Coordinates Country, territory or ocean Notes
60°0′N 0°0′E / 60.000°N 0.000°E / 60.000; 0.000 (Prime Meridian) Atlantic Ocean North Sea
60°0′N 5°3′E / 60.000°N 5.050°E / 60.000; 5.050 (Norway)  Norway Islands of Stolmen and Selbjørn, Hordaland
60°0′N 5°12′E / 60.000°N 5.200°E / 60.000; 5.200 (Prime Meridian) Atlantic Ocean Bekkjarviksundet, Selbjørnsfjorden, North Sea
60°0′N 5°15′E / 60.000°N 5.250°E / 60.000; 5.250 (Norway)  Norway Island of Huftarøy, Hordaland
60°0′N 5°17′E / 60.000°N 5.283°E / 60.000; 5.283 (Prime Meridian) Atlantic Ocean Langenuen, North Sea
60°0′N 5°22′E / 60.000°N 5.367°E / 60.000; 5.367 (Norway)  Norway Islands of Reksteren, Tysnesøy and the mainland Hordaland
60°0′N 5°52′E / 60.000°N 5.867°E / 60.000; 5.867 (Prime Meridian) Atlantic Ocean Hardangerfjorden, North Sea
60°0′N 5°59′E / 60.000°N 5.983°E / 60.000; 5.983 (Norway)  Norway Mainland: Folgefonna glacier, Telemark, Buskerud, Akershus, Oslo, Hedmark, Østfold
Passing just north of the capital Oslo
60°0′N 12°23′E / 60.000°N 12.383°E / 60.000; 12.383 (Sweden)  Sweden Passing through Fagersta
Passing just north of Uppsala
60°0′N 18°53′E / 60.000°N 18.883°E / 60.000; 18.883 (Baltic Sea) Atlantic Ocean Baltic Sea
60°0′N 20°8′E / 60.000°N 20.133°E / 60.000; 20.133 (Åland Islands)  Finland Högskär, Bäckö and several smaller islands,  Åland Islands
60°0′N 20°58′E / 60.000°N 20.967°E / 60.000; 20.967 (Baltic Sea) Atlantic Ocean Baltic Sea
60°0′N 23°30′E / 60.000°N 23.500°E / 60.000; 23.500 (Finland)  Finland Passing through Ekenäs
60°0′N 23°58′E / 60.000°N 23.967°E / 60.000; 23.967 (Baltic Sea) Atlantic Ocean Baltic Sea
60°0′N 24°26′E / 60.000°N 24.433°E / 60.000; 24.433 (Finland)  Finland Porkkala peninsula
60°0′N 24°30′E / 60.000°N 24.500°E / 60.000; 24.500 (Baltic Sea) Atlantic Ocean Baltic Sea, Gulf of Finland
Passing just south of Helsinki,  Finland and the island of Gogland,  Russia
60°0′N 27°48′E / 60.000°N 27.800°E / 60.000; 27.800 (Russia)  Russia Moshchny Island
60°0′N 27°54′E / 60.000°N 27.900°E / 60.000; 27.900 (Baltic Sea) Atlantic Ocean Gulf of Finland, Baltic Sea
60°0′N 29°44′E / 60.000°N 29.733°E / 60.000; 29.733 (Russia)  Russia Island of Kotlin (city of Kronstadt)
60°0′N 29°47′E / 60.000°N 29.783°E / 60.000; 29.783 (Baltic Sea) Atlantic Ocean Gulf of Finland, Baltic Sea
60°0′N 30°5′E / 60.000°N 30.083°E / 60.000; 30.083 (Russia)  Russia Passing through Saint Petersburg, Lake Ladoga
60°0′N 154°30′E / 60.000°N 154.500°E / 60.000; 154.500 (Sea of Okhotsk) Pacific Ocean Shelikhov Gulf, Sea of Okhotsk
60°0′N 161°28′E / 60.000°N 161.467°E / 60.000; 161.467 (Russia)  Russia Kamchatka Peninsula
60°0′N 165°14′E / 60.000°N 165.233°E / 60.000; 165.233 (Bering Sea) Pacific Ocean Bering Sea
60°0′N 166°10′E / 60.000°N 166.167°E / 60.000; 166.167 (Russia)  Russia Pylgin Range
60°0′N 166°33′E / 60.000°N 166.550°E / 60.000; 166.550 (Bering Sea) Pacific Ocean Olyutor Gulf, Bering Sea
60°0′N 170°9′E / 60.000°N 170.150°E / 60.000; 170.150 (Russia)  Russia Olyutor Peninsula
60°0′N 170°26′E / 60.000°N 170.433°E / 60.000; 170.433 (Bering Sea) Pacific Ocean Bering Sea
60°0′N 167°8′W / 60.000°N 167.133°W / 60.000; -167.133 (United States)  United States Alaska - Nunivak Island
60°0′N 165°39′W / 60.000°N 165.650°W / 60.000; -165.650 (Etolin Strait) Pacific Ocean Etolin Strait, Bering Sea
60°0′N 164°9′W / 60.000°N 164.150°W / 60.000; -164.150 (United States)  United States Alaska
60°0′N 152°38′W / 60.000°N 152.633°W / 60.000; -152.633 (Cook Inlet) Pacific Ocean Cook Inlet, Gulf of Alaska
60°0′N 151°44′W / 60.000°N 151.733°W / 60.000; -151.733 (United States)  United States Alaska - Kenai Peninsula, Evans Island, Elrington Island, Latouche Island and Montague Island
60°0′N 147°24′W / 60.000°N 147.400°W / 60.000; -147.400 (Pacific Ocean) Pacific Ocean Gulf of Alaska
60°0′N 144°24′W / 60.000°N 144.400°W / 60.000; -144.400 (United States)  United States Alaska - Wingham Island, Kayak Island and a small section of mainland
60°0′N 143°50′W / 60.000°N 143.833°W / 60.000; -143.833 (Pacific Ocean) Pacific Ocean Gulf of Alaska
60°0′N 141°53′W / 60.000°N 141.883°W / 60.000; -141.883 (United States)  United States Alaska
60°0′N 139°3′W / 60.000°N 139.050°W / 60.000; -139.050 (Canada)  Canada Yukon / British Columbia border
Northwest Territories / British Columbia border
Northwest Territories / Alberta border - passes through Wood Buffalo National Park and beside Fort Smith, NT
Northwest Territories / Saskatchewan border
Nunavut / Manitoba border
60°0′N 94°49′W / 60.000°N 94.817°W / 60.000; -94.817 (Hudson Bay) Arctic Ocean Hudson Bay
Passing just north of the Ottawa Islands, Nunavut,  Canada
60°0′N 77°17′W / 60.000°N 77.283°W / 60.000; -77.283 (Canada)  Canada Quebec
Passing just south of Puvirnituq, Quebec
60°0′N 69°46′W / 60.000°N 69.767°W / 60.000; -69.767 (Ungava Bay) Arctic Ocean Ungava Bay
Passing just south of Kangirsuk, Quebec,  Canada
60°0′N 65°7′W / 60.000°N 65.117°W / 60.000; -65.117 (Canada)  Canada Quebec, Newfoundland and Labrador
60°0′N 64°9′W / 60.000°N 64.150°W / 60.000; -64.150 Atlantic Ocean Border between the Davis Strait (to the north) and the Labrador Sea (to the south)[5]
60°0′N 44°52′W / 60.000°N 44.867°W / 60.000; -44.867 (Greenland)  Greenland Passing south of Narsaq; crossing mainland at Narsarmijit; going through Cape Farewell Archipelago, passing just north of Itilleq Island
60°0′N 43°9′W / 60.000°N 43.150°W / 60.000; -43.150 (Atlantic Ocean) Atlantic Ocean
60°0′N 1°21′W / 60.000°N 1.350°W / 60.000; -1.350 (United Kingdom)  United Kingdom Islands of Mainland and Mousa, Shetland Islands,  Scotland
60°0′N 1°11′W / 60.000°N 1.183°W / 60.000; -1.183 (North Sea) Atlantic Ocean North Sea

Notable cities and towns on 60°N

[edit]

Canada

[edit]
The 60th parallel north in Canada, marking the southern borders of Yukon, Northwest Territories, and the Nunavut mainland.

In Canada, the 60th parallel forms the southern mainland boundary of the northern territories of Yukon, Northwest Territories, and Nunavut with the western provinces of British Columbia, Alberta, Saskatchewan, and Manitoba.

Accordingly, "north of 60" is an expression often used for the territories, although parts of Nunavut (the islands in Hudson Bay and James Bay) are located south of the 60th parallel, and parts of Quebec and Newfoundland and Labrador are located north, to the east of Hudson Bay. A 1990s TV show on CBC about life in the Northwest Territories was called North of 60.

The 60th Parallel Territorial Park is on Mackenzie Highway between Alberta and Northwest Territories and it has a visitor centre there in the homeland of the Yellowknives Dene First Nation and the North Slave Métis Alliance.[6]

Canada's only four corners are located at the intersection of the 60th parallel and the 102nd meridian west, between the Northwest Territories, Nunavut, Saskatchewan, and Manitoba.

Greenland

[edit]

Between 1776 and 1950, the 60th parallel formed the southern limit of the Royal Greenland Trade Department's exclusive monopoly on trade near the Dano-Norwegian and later Danish colonies of Greenland (1776–1782) and South Greenland (1782–1950).[7]

See also

[edit]

References

[edit]
Revisions and contributorsEdit on WikipediaRead on Wikipedia

60th parallel north

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The 60th parallel north is a encircling at 60 degrees north of the , a standard measure of used in and to denote positions relative to the planet's rotational axis. Due to 's spherical shape, this parallel has a of approximately 20,038 kilometers, roughly half that of the , as the radius decreases with increasing according to the cosine of the angle from the . This parallel traverses diverse geographical regions, beginning in the North near the (), then crossing the Islands in () before entering mainland . In , it passes through near the city of (at 60.39° N), central , and southern close to (at 60.17° N). Further east, it cuts across northwestern north of (59.93° N), then crosses marginal seas (Barents, Kara, Laptev, and East Siberian Seas) before re-entering land in eastern in Chukotka and the northern , and enters the east of Kamchatka. It then crosses the into , traversing southern () south of Anchorage, forms the southern boundary of Canada's , , and , and continues through , northern , and before entering the and reaching southern () in its southern fjords, returning to the North Atlantic. The 60th parallel marks significant geopolitical and environmental boundaries. In Canada, it delineates the divide between the southern provinces and the northern territories, influencing administrative, , and spill response regimes, with distinct policies applying north of this line for Arctic sovereignty and . In , it approximates the southern extent of continuous , affecting infrastructure planning, wildlife habitats, and ecosystems, as permafrost distribution thins and becomes discontinuous south of this latitude. Across , the parallel aligns with the transition from temperate to climates, where boreal forests dominate and growing seasons shorten, impacting , , and biodiversity in regions like and . Notable settlements along or near the parallel include , , Whitehorse (, ), and Fort Smith (, ), highlighting its role in patterns in high-latitude environments. Astronomically and culturally, the 60th parallel experiences extreme seasonal variations, with summer days exceeding 18 hours of daylight and winter nights similarly prolonged, though it lies south of the (66° 34' N) where true polar day and night occur. This positioning places it within the auroral oval, making northern lights visible during geomagnetic activity, particularly in Scandinavian and Alaskan segments. Historically, the parallel has served as a reference for and mapping, from Viking voyages in the North Atlantic to modern resource development, underscoring its importance in global connectivity amid pressures on polar regions.

Geographical Overview

Definition and Characteristics

The 60th parallel north is a located 60 degrees north of the , encircling the as an imaginary line parallel to the equatorial plane. This parallel represents an angular measurement from the 's center, where is defined by the angle between the equatorial plane and the line connecting the point on the surface to the center of the . Due to the 's oblate shape, the distance along a meridian from the to the 60th parallel north is approximately 6,667 kilometers. The length of the parallel itself, calculated as the at that , is about 20,038 kilometers, roughly half the equatorial of 40,075 kilometers, because the at 60 degrees north is reduced by the cosine of 60 degrees (0.5). In global , the 60th parallel north holds significance as a marker in systems, often delineating the approximate boundary between temperate and zones, particularly in continental interiors where it separates humid continental climates from harsher conditions typically spanning 50 to 70 degrees north. It also plays a role in and , serving as a reference line for mapping polar and high-latitude regions, and in some geopolitical contexts, such as defining the southern extent of territories in . Additionally, it contributes to broader definitions of polar regions in environmental and scientific studies, highlighting transitions in ecosystems and atmospheric dynamics. Locations along the 60th parallel north exhibit pronounced seasonal variations in day length due to the Earth's of 23.5 degrees, resulting in extended daylight during summer and shortened days in winter, though without the full polar day or night phenomena seen farther north. On the around June 21, daylight lasts approximately 18 hours and 53 minutes, while on the around December 21, it is reduced to about 5 hours and 7 minutes. These extremes influence local , activities, and cycles, with summer providing near-continuous for much of the day and winter featuring prolonged that affects and .

Global Path Summary

The 60th parallel north forms a complete circuit around the Earth at 60 degrees latitude, beginning at the Prime Meridian in the North Sea of the Atlantic Ocean. Proceeding eastward, it first crosses the Shetland Islands in the United Kingdom, then traverses mainland Norway, Sweden, and Finland before entering Russia north of St. Petersburg. It continues through western Russia and across Siberia, reaching the Kamchatka Peninsula around 160° E longitude. The parallel then enters the Pacific Ocean, crossing the northern Pacific Ocean, the Bering Sea, and the Gulf of Alaska before making landfall in Alaska near Seward. From there, it follows through the Yukon Territory and Northwest Territories, passing south of Whitehorse, forming the northern boundaries of British Columbia, Alberta, Saskatchewan, and Manitoba, crossing northern Ontario and Quebec, entering Labrador, and reaching the Atlantic coast in southern Labrador. It then crosses Hudson Bay, enters northern Quebec, continues through Labrador to the Atlantic, crosses the Labrador Sea, enters southern Greenland's fjords, and returns to the North Atlantic via the Davis Strait. Along its approximately 20,000 km length, the parallel spends roughly two-thirds over land—across , (including and ), and —and one-third over ocean, with major crossings of the Atlantic and Pacific Oceans as well as waters in and the ; it intersects three principal landmasses (, , and ) and several oceanic regions. Elevation along the parallel varies significantly, from in oceanic segments and coastal areas to over 1,600 meters at peaks such as the Folgefonna glacier in , where the highest point reaches 1,662 meters above . The parallel lies about 3,333 km south of the , calculated as 30 degrees of at an average of 111 km per degree. It also serves as the southern boundary for certain definitions of the region, such as in , where territories north of the 60th parallel are considered part of the Canadian .

Continental Crossings

European Segment

The 60th parallel north enters the European continent from the Atlantic Ocean by crossing the Shetland Islands, part of the , where it passes through the archipelago's southern reaches, including areas near Mousa Island. From there, the parallel continues eastward into the before making landfall on mainland near the islands of Stolmen and Selbjørn in county, approximately at 60°00′N 5°12′E. In , it traverses a rugged coastal landscape characterized by fjords and steep terrain, heading inland through the western fjord systems and approaching the Folgefonna glacier in the Hardanger region, where it skirts the glacier's southern margins around 60°00′N 6°20′E. Further east in Norway, the parallel passes just south of Bergen on the west coast, at about 60°23′N, before cutting through the coastal mountains and valleys of the Scandinavian interior, eventually passing just north of Oslo, located at 59°55′N. This segment highlights the transition from maritime-influenced fjords to the more continental upland plateaus of the Scandinavian Mountains, with elevations rising to over 1,000 meters in places along the route. The parallel then crosses into Sweden near Fagersta, at precisely 60°00′N 15°46′E, weaving through central Sweden's dense boreal forests, numerous lakes, and rolling hills. It continues northeast, passing just north of Uppsala at 59°51′N, before entering Finland. In Finland, the path first crosses the autonomous Åland Islands archipelago around 60°00′N 20°00′E, then proceeds over the mainland near Ekenäs (Tammisaari) at 59°58′N and the Porkkala Peninsula at 60°00′N 24°30′E, approaching the Gulf of Finland amid forested coastal lowlands and Baltic Sea inlets. Throughout its European traversal, the 60th parallel encounters diverse natural features, including the glaciated peaks and valleys of the in , expansive coniferous forests and freshwater systems in , and archipelagic waters transitioning to the approaches in . The total land distance covered in Europe spans approximately 2,500 km, from the Shetland Islands to the eastern . The parallel exits European territory toward via Moshchny Island at 60°00′N 27°50′E and near on at 59°59′N 29°46′E, entering the broader eastern Baltic region.

Asian Segment

The 60th parallel north enters the Asian portion of Russia at the , marking the conventional boundary between and , in Sverdlovsk Oblast near the town of Karpinsk. From there, it traverses the expansive , a vast lowland region characterized by low-relief terrain, wetlands, and boreal forests known as . This segment spans several oblasts, including and Khanty-Mansi, crossing major rivers such as the Ob, which flows northward through the plain, and the Tura, a in the Ob basin. Continuing eastward for over 8,000 kilometers across , the parallel moves through the , where elevations rise modestly to form rolling plateaus and dissected uplands covered in dense of coniferous trees like , , and . It intersects significant northward-flowing rivers, including the Yenisei near its middle course around 89° E longitude, and the Lena farther east in the , contributing to the region's intricate drainage systems that support diverse aquatic ecosystems. As it progresses, the landscape transitions toward the edges of zones, with discontinuous becoming prevalent, leading to phenomena like lakes and cryosols that influence soil stability and vegetation patterns. In the , the parallel cuts through remote, rugged areas of and the former Koryak Autonomous Okrug, now part of , skirting volcanic terrains associated with the . It passes over the Olyutor Peninsula, a protruding landform on the northeastern coast of Kamchatka, before reaching the approaches to Shelikhov Gulf. The Asian segment concludes as the parallel exits the continent into the , a marginal sea of the known for its cold currents and seasonal ice cover.

North American Segment

The 60th parallel north enters from the across the , reaching . , located approximately 60 miles offshore from the Yukon-Kuskokwim Delta, marks the first significant land crossing in the United States, where the parallel traverses the island's varied terrain of tundra and low hills. From there, the parallel continues eastward through the , with no further land crossings until it reaches the , where it passes over Wingham Island (60°03′N 144°24′W) and Kayak Island (near 60°00′N 144°22′W), along with a small section of mainland near Controller Bay. In , the parallel then crosses a short segment of the before intersecting the south of communities like Ninilchik and Seward, where the landscape transitions into temperate coastal rainforests and rugged fjords characteristic of the Kenai Fjords area. The Alaskan segment features a mix of maritime influences, with dense spruce-hemlock forests along the coast giving way to alpine meadows and glaciated valleys inland, spanning roughly the longitudinal range from 166°W to 141°W. This portion highlights the dramatic contrast between Alaska's coastal ecosystems and the encroaching mountainous barriers of the range. The parallel then crosses into Canada at the Alaska-Yukon border near 141°W, where it aligns with the international boundary before becoming the southern demarcation of . As it progresses eastward, it forms the between and , then shifts to delineate the from and around 120°W. In this region, the parallel traverses the western edges of , a vast protected area spanning the Alberta- boundary, encompassing boreal wetlands, sand dunes, and landscapes. The terrain here reflects the transition from the Cordilleran uplands to the expansive , with the parallel passing through coniferous forests and sinkholes that support diverse wildlife habitats. Continuing through central Canada, the 60th parallel crosses the prairie provinces of , , and , where it bisects agricultural lowlands interspersed with boreal forest fringes and lakes such as those in the Manitoba Escarpment region. Features include expansive aspen parklands and shallow wetlands that feed into the , with the parallel crossing before re-entering land in northern near on the eastern coast. In , it approaches the Manitoba-Nunavut border near the Churchill River system, marking a shift to more sparsely vegetated and permafrost-influenced soils. The interior Canadian landscape along this route exemplifies the boreal zone's ecological gradient, from edges in the prairies to dense black spruce stands and lakes further north. Eastward, the parallel proceeds across the in northern , characterized by rolling plateaus and river valleys, before crossing into . In , the parallel traverses the remote interior of the Labrador Plateau, featuring ancient rock formations and sparse vegetation adapted to long winters. The total land traversal across [North America](/page/North America) along this parallel approximates 4,000 kilometers, encompassing diverse physiographic provinces from coastal archipelagos to continental interiors.

Oceanic and Arctic Crossings

Atlantic Ocean Traverses

The 60th parallel north crosses the in distinct eastern and western segments, reflecting the ocean's division by continental landmasses. In the eastern Atlantic, the parallel begins in the near the , approximately at 60° N, 0° longitude, and proceeds westward across open waters before approaching the Islands, whose main settlement of lies at 60°09′ N. This segment includes margins of the , where the parallel skirts the northern edges of the sea before intersecting land in the . In the western Atlantic, the parallel emerges from the approaches to Ungava Bay in northern , , around 60° N, 65° W, and traverses the , which forms the boundary with the to the south. It continues through the strait, separating from southwestern , until reaching the Cape Farewell Archipelago near 60° N, 42° W, just north of Greenland's southernmost point. These Atlantic traverses occur over deep oceanic waters, with average depths of about 3.6 kilometers, characteristic of the North Atlantic basin's abyssal plains and mid-ocean ridges. The northern reaches along the 60th parallel are notably influenced by the system, which extends northward as the , transporting warm subtropical waters toward and moderating temperatures in otherwise latitudes. This current's vestiges reach as far north as 60° N, contributing to relatively milder winters in adjacent coastal regions compared to similar latitudes without such oceanic warming. The combined length of the eastern and western segments totals approximately 3,500 kilometers, encompassing both the confined passages like the and the broader open-ocean expanse. From a nautical perspective, the 60th parallel's Atlantic segments play a role in transatlantic shipping routes connecting and , particularly northern variants that follow great-circle paths to optimize distance for destinations like ports in or the Canadian Arctic. Vessels navigating these waters, especially near Greenland's Cape Farewell, must contend with icebergs calved from glaciers and carried southward by the , posing hazards that require vigilant ice monitoring and routing adjustments. As of 2024, declining in adjacent regions has extended navigable periods but increased risks from variable ice conditions.

Pacific Ocean Traverses

The 60th parallel north enters the in its western segment by crossing into the northern from the Russian mainland, passing through the expansive Shelikhov Gulf, a northeastern arm of the sea extending northward between the Siberian coast and the . This gulf, reaching depths of 100 to 150 meters on average, features narrow passages prone to extreme tidal ranges exceeding 10 meters in adjacent Penzhina Bay, contributing to turbulent conditions and high waves amplified by strong winds and funneling effects in the confined . The parallel then continues eastward across the broader northern before reaching the , after which it re-enters the ocean via the Olyutor Gulf on the side, a coastal indentation along the peninsula's eastern flank at approximately 60°N, 170°E. These western passages are subject to , including storms that generate significant wave heights, making navigation challenging in this remote region. In the central Pacific, the parallel traverses the open expanse of the , spanning roughly 1,500 kilometers east-west at this between the and the Alaskan coast. This crossing occurs amid waters influenced by the North Pacific Subarctic Gyre, a cyclonic circulation system that drives nutrient and connects transitional waters between the subtropical Pacific and the via the . During winter months, the region experiences extensive floating coverage, with pack ice extending southward to around 60°N, impacting marine transport and ecosystems through seasonal freezing that can reach thicknesses of up to 1.5 meters in severe years. As of 2024, ice extent has declined by about 13% per decade since 1979, altering seasonal patterns. The eastern segment sees the parallel entering the , a broad embayment shaped by the —a branch of the —before crossing into the lower reaches of , a glacially carved system with depths up to 300 meters and strong tidal bores. These waters are dynamically influenced by the Aleutian North Current, which flows northward along the continental margin, fostering high productivity through mixing of fresh glacial runoff and saline oceanic inflows. The overall Pacific traversal along the 60th parallel encompasses diverse marine environments supporting rich fisheries, particularly for Pacific salmon species like chinook and sockeye, as well as snow and populations in the , which sustain major commercial harvests yielding tens of thousands of metric tons annually. Near the Asian margins, the region faces risks from typhoons transitioning into extratropical storms, capable of producing waves over 8 meters and heavy precipitation impacting coastal areas like Kamchatka.

Arctic and Hudson Bay Regions

The 60th parallel north enters from the eastern Canadian coast in , traversing approximately 1,500 km of the bay's expansive brackish waters before reaching the western shore near . These waters exhibit low salinity, primarily due to substantial freshwater inflows from major rivers such as the Nelson and Churchill, which contribute an annual average of about 0.9 meters of freshwater to overall, creating pronounced stratification and estuarine conditions. Semidiurnal of Atlantic origin propagate counterclockwise into the bay via , influencing coastal dynamics and mixing zones along this latitudinal path. (Delphinapterus leucas) populations in the western stock were estimated at around 23,000 during the late 1980s; as of the 2010s, the population is approximately 57,000 (CV=0.21). These whales utilize these areas extensively, with large summer aggregations forming in the estuary for calving and feeding before migrating northward in fall to overwinter in . Ungava Bay, a narrow inlet approximately 260 km wide at its mouth and situated between Quebec and Labrador, is crossed by the 60th parallel, which runs through its central portions amid steep, irregular shores rising abruptly from depths reaching up to 300 meters near the Atlantic entrance. The bay's fjord-like coastal morphology, characterized by relatively steep slopes along much of the northern Ungava Peninsula, results from Precambrian Shield geology and glacial erosion, forming rugged headlands and small islands that shelter inshore habitats. Freshwater discharges from rivers like the Koksoak further reduce salinity in the inner bay, supporting a mix of Arctic and subarctic marine species adapted to variable estuarine conditions. In the broader Arctic margins, the 60th parallel approaches the northern edges of Baffin Bay between and , where it delineates transitions into colder waters with nearly complete seasonal ice cover during winter months, often exceeding 80% extent and persisting until spring breakup influenced by regional and formation. These ice dynamics in Baffin Bay's southern approaches create vital habitats for marine mammals and seabirds, while low-salinity plumes from coastal runoff enhance productivity in ice-free summer periods. Overall, the parallel's path through these enclosed basins and inland seas totals about 2,000 km of water, dominated by hydrological features like freshwater inflows that maintain brackish profiles across the region.

Human Geography

Notable Settlements

The 60th parallel north traverses or lies in close proximity to several notable settlements across , , , and , many of which function as key ports, administrative hubs, or cultural centers in environments. These locations highlight the parallel's role in connecting coastal and inland communities adapted to and variable maritime influences. Globally, major settlements along this line remain sparse, with fewer than 50 significant urban centers due to the challenging and . In the European segment, , (60.39° N), stands as a prominent coastal port renowned for its access and historical trade role. Nearby, , (59.91° N), serves as a vibrant cultural hub with museums and theaters emphasizing Nordic heritage. , (60.17° N), the capital at the parallel, operates as a modern tech center fostering innovation in design and digital industries. , (59.93° N), positioned on the , is a historic city featuring imperial architecture and waterways central to its identity. , (59.85° N), functions as a longstanding town, home to one of Scandinavia's oldest academic institutions. Shifting to North America, , , (60.72° N), acts as the territorial capital, coordinating regional governance and transportation in the interior. , (60.00° N), exactly on the parallel, operates as a gateway town facilitating access to and northern trade routes. , (60.55° N), represents a coastal fishing community focused on harvesting and along . In , (60.91° N) emerges as a southern settlement emphasizing traditional and local resource-based economies near the Arctic Circle's edge. These settlements collectively underscore the parallel's influence on human activity, where maritime connectivity and administrative functions prevail amid subarctic adaptations like insulated infrastructure and seasonal economies.

Population Distribution

The 60th parallel north traverses regions of exceptionally low human population density, with a global average of less than 1 person per square kilometer along its path, reflecting the challenges of high-latitude environments. In the European segment, densities are comparatively higher at 10–20 persons per km² in coastal and southern areas of Norway, Sweden, and Finland, where milder subarctic conditions and historical settlement patterns support denser habitation. By contrast, the Asian segment in Siberia exhibits densities below 0.1 persons per km², due to vast taiga and tundra expanses with minimal infrastructure. In North America, densities along the parallel in Alaska and Canada average under 0.5 persons per km², while the Greenlandic portion remains even sparser at approximately 0.03 persons per km² overall. Regional population estimates in areas north of or bordering the parallel highlight stark disparities, with approximately 5 million people in European proximity as of 2021—primarily in southern and coastal —contrasting with 1–2 million in Russian territories like as of 2021. North American figures for such regions total around 774,000 as of 2025, dominated by Alaskan communities north of the parallel (approximately 640,000 north of 60° N out of a statewide total of about 740,000) and Canadian territorial populations totaling about 134,500 across (48,000), (45,000), and (41,500). contributes roughly 10,000 residents in southern coastal settlements like near the parallel as of 2025. Settlement patterns are heavily influenced by harsh subarctic and arctic climates, which limit agriculture and permanent habitation to less than 10% of the land in many areas, concentrating populations near coasts for access to marine resources and transportation routes. Resource extraction, including oil, gas, and mining, drives localized clusters, such as in Norway's Tromsø region or Russia's , while indigenous groups like the Sami in and in and maintain traditional livelihoods adapted to these environments, comprising 5–20% of local populations in affected territories. Population trends show slow overall growth in resource-dependent towns, with annual increases of 1–2% in Alaskan and some Scandinavian settlements due to economic opportunities, offset by southward that draws younger residents to southern urban centers for better services and employment. In Siberian and Canadian northern territories, net migration remains negative or stagnant, contributing to aging demographics and limited expansion beyond existing hubs.

Political and Historical Aspects

Territorial Boundaries

The 60th parallel north serves as a significant administrative boundary in Canada, forming the southern limit of the mainland portions of the three northern territories: , , and . This demarcation separates these territories from the provinces of to the west, , , and to the south. At approximately 60°N 102°W, the parallel intersects with the 102nd meridian , creating Canada's only where four jurisdictions meet: , , , and . An exception to this mainland boundary applies to Nunavut, which extends southward to include all islands in , , and Ungava Bay that lie south of the 60th parallel, provided they are not part of , , or . Portions of and extend north of the parallel, incorporating coastal areas and islands beyond the standard territorial divide. In , the 60th parallel traverses numerous federal subjects across its European and Asian extents, through regions such as the , , , , , , and in the central Ural area, extending eastward to , , and ultimately in the far east. These crossings primarily define internal administrative lines rather than international borders, facilitating regional without altering national frontiers. Elsewhere, the parallel marks the southern tip of Greenland (Denmark), with no active international borders. In Europe, it passes through the Shetland Islands of the United Kingdom, representing the northernmost extent of British territory at approximately 60°N.

Historical Significance

The 60th parallel north has been a pivotal line in the history of exploration, marking pathways for early seafaring and overland expansions. During the Viking Age (9th to 11th centuries), Norse explorers from Scandinavia established key routes and settlements near the parallel, notably in the Shetland Islands at approximately 60°10′N, which served as a vital base for voyages across the North Atlantic toward Iceland, Greenland, and beyond. These settlements, beginning around 850 AD, facilitated trade in furs, walrus ivory, and slaves, while also enabling raids on mainland Europe. In the 16th century, Russian Cossacks under Yermak Timofeyevich crossed the parallel during their 1581–1582 campaign against the Khanate of Sibir, defeating Khan Kuchum at the Irtysh River and securing western Siberia for the Tsardom of Russia; this conquest initiated a 300-year expansion that incorporated Siberian territories north of 60°N into the Russian Empire through fur trade outposts and military forts. The colonial era further highlighted the parallel's role in trade monopolies and territorial disputes. From 1776 to 1950, the Danish-Norwegian government enforced a monopoly in southern via the Royal Greenland Trading Department, restricting foreign commerce to protect Inuit communities and extract resources like and hides, which isolated the region economically until reforms post-World War II. Meanwhile, in the North Atlantic, the Islands—under Norse control for nearly 600 years—were pledged to the Scottish crown in 1469 as security for a royal dowry, effectively transferring British claims over the archipelago and ending direct Scandinavian sovereignty along the parallel. In the 20th century, the parallel gained strategic importance in aviation and military conflicts. Early transpolar flights, such as Soviet pilot Valery Chkalov's 1937 nonstop journey in an ANT-25 from Moscow to Vancouver—covering 5,500 miles and crossing Arctic latitudes near 60°N—demonstrated the feasibility of aerial routes over the pole, paving the way for commercial polar aviation. During the Cold War (1946–1991), the United States established bases like Elmendorf Air Force Base near Anchorage, Alaska (61°13′N), for air defense against Soviet incursions, while Norway built extensive bunker networks in its northern regions around Tromsø (69°N) to support NATO operations and monitor submarine activity in the Barents Sea. Modern developments since the 1970s have centered on resource extraction and international cooperation. The 1968 discovery of the Prudhoe Bay oil field in Alaska (70°15′N but with infrastructure extending south toward 60°N) triggered an oil boom, culminating in the 1977 completion of the 800-mile Trans-Alaska Pipeline, which boosted state revenues and spurred economic growth along northern latitudes. In Canada, mining north of 60°N expanded significantly post-1970s, with major projects like the Ekati diamond mine (opened 1998 in the Northwest Territories) and gold operations in Yukon driving territorial economies through federal incentives and infrastructure investments. The establishment of the Arctic Council in 1996 as an intergovernmental forum among eight Arctic states has since prioritized climate change discussions, addressing impacts like permafrost thaw and sea ice loss in regions encompassing the 60th parallel to promote sustainable development.

Climate and Environment

Climatic Patterns

The 60th parallel north lies predominantly within the zone, characterized by annual average temperatures ranging from 0°C to 10°C, with significant regional variations driven by continental versus maritime influences. In coastal areas of and , moderated by currents, averages hover around 2°C to 7°C, while inland Siberian locations experience colder means near 0°C or below. Winters are severe, with average temperatures typically between -10°C and -30°C, dropping lower in continental interiors due to limited maritime moderation, whereas coastal regions see milder lows around -5°C to -15°C. Summers are cool and brief, with averages of 10°C to 20°C, reaching up to 18°C to 20°C along European coasts and 15°C in Alaskan coastal zones, fostering short growing seasons of 1 to 3 months where temperatures exceed 10°C./The_Physical_Environment_(Ritter)/09:_Climate_Systems/9.06:_High_Latitude_Climates/9.6.01:_Subarctic_Climate) Precipitation along the parallel totals 500 to 1,000 mm annually in most areas, though it exceeds 2,000 mm on windward west coasts exposed to prevailing , such as in where enhances . In contrast, inland Siberian segments receive 400-700 mm in the west, decreasing to under 300 mm further east, primarily as snow. Snowfall dominates winter across the parallel, accumulating 50-200 cm in coastal areas like and , and 100-400 cm in continental areas, varying by location and frequency. Summer is more evenly distributed as , supporting limited vegetation growth despite the cool conditions. Seasonal variations are pronounced, with long winters lasting 6 to 8 months from to or May, during which daylight is limited and the often intensifies cold outbreaks by steering Arctic air southward across the parallel. The short summers, from to , feature extended daylight but persistent cool temperatures, limiting frost-free periods to 60 to 90 days in many locations. Ocean currents play a key role in these patterns: the North Atlantic extension of the warms European segments, preventing deep freezes and enabling ice-free ports, while the colder Pacific influences result in greater temperature extremes along Alaskan and eastern Russian coasts compared to the Atlantic side. Climate extremes underscore the parallel's harsh conditions, with record lows approaching -50°C in Siberian interiors during disruptions, as seen in locations like where temperatures have plummeted to -59°C. Highs rarely exceed 30°C, even in summer peaks. Tropical hurricanes are rare at this due to cold sea surface temperatures, but extratropical nor'easters and intense cyclones frequently impact Atlantic segments, bringing heavy snow and winds exceeding 100 km/h to coastal and Greenlandic waters. Due to Arctic amplification, regions along the 60th parallel have warmed at 2-3 times the global average rate, with 2024-2025 marking record high temperatures in the and increased falling as rain rather than snow. This has led to thaw, more frequent wildfires, and shifts in zones, impacting ecosystems and infrastructure as of November 2025.

Ecological Features

The 60th parallel north traverses diverse ecological zones, primarily the vast circumpolar boreal forest () on land, interspersed with transitions and productive marine environments in the Pacific and Atlantic Oceans. This latitude marks a boundary where coniferous-dominated forests give way to in higher elevations or northern extents, supporting resilient ecosystems adapted to short growing seasons, cold temperatures, and nutrient-poor soils. The boreal zone here stores significant carbon in peatlands and , playing a critical role in global climate regulation, while marine segments feature nutrient-rich that sustains fisheries. In North American segments, particularly through and , the parallel crosses the Taiga Plains and Boreal Cordillera ecoregions, characterized by open stands of black spruce (), white spruce (), jack pine (), and deciduous species like trembling aspen () and white birch (). These forests transition to shrublands with dwarf birch (Betula glandulosa) and lichens near the , supported by in areas and numerous wetlands that enhance . Wildlife includes large herbivores such as (Alces alces) and woodland caribou (Rangifer tarandus caribou), predators like gray wolves () and (Lynx canadensis), and migratory birds including snow geese (Anser caerulescens) and common loons (Gavia immer), which rely on the region's lakes and rivers for breeding. European portions, spanning , , and , feature middle and northern boreal forests with (Picea abies), (Pinus sylvestris), and downy birch (Betula pubescens), influenced by the warming that extends treeline viability southward compared to continental interiors. These ecosystems host brown bears (Ursus arctos), (Lynx lynx), and capercaillie (Tetrao urogallus), with diverse understory lichens and mosses supporting (Rangifer tarandus) herds. In , along the parallel through and , the expands into the world's largest contiguous forest, dominated by Siberian pine (Pinus sibirica), Siberian fir (Abies sibirica), and (Larix sibirica) in eastern reaches, sustaining (Capreolus pygargus), brown bears (Ursus arctos), and vast bird populations like the (Perisoreus infaustus). These forests cover approximately 12 million km² globally, with key ecological processes like fire regeneration maintaining . Oceanic traverses include the North Pacific, a high-nutrient, low-chlorophyll region limited by iron, fostering blooms that underpin ( spp.) runs and marine mammals like sea otters ( lutris). In the segment of the Atlantic, Atlantic water inflows create a productive with blooms supporting (Gadus morhua), Norwegian (Clupea harengus), and marine mammals such as minke whales ( acutorostrata), enhanced by seasonal and a diverse benthic community. These marine areas contribute to global oxygen production and , linking terrestrial and oceanic food webs along the parallel.

References

  1. https://oceanservice.noaa.gov/facts/latitude.html
  2. https://people.ohio.edu/dyer/TPE/tpe_3e/essentials/locational_systems.html
  3. https://www.adn.com/alaska-life/we-alaskans/2017/02/05/circling-the-globe-at-60-degrees-north-sampling-the-people-and-places/
  4. https://www.mapsofworld.com/lat_long/norway-lat-long.html
  5. https://www.mapsofworld.com/lat_long/helsinki.html
  6. https://dot.alaska.gov/comm/pressbox/arch_2016/PR16-1023.shtml
  7. https://central.bac-lac.canada.ca/.item/?id=rcap-534&app=Rcap&op=pdf
  8. https://tc.canada.ca/en/follow-audit-ship-source-spills
  9. https://dggs.alaska.gov/webpubs/outside/text/dnag_ch28.pdf
  10. https://pubs.usgs.gov/pp/0628/report.pdf
  11. https://www.nationalgeographic.com/science/article/auroras
  12. https://www.nationalgeographic.com/science/article/alaska-has-finally-been-mapped-as-precisely-as-mars
  13. https://www.thoughtco.com/degree-of-latitude-and-longitude-distance-4070616
  14. https://www.oneoceanexpedition.com/ocean-education/latitude-and-longitude-and-other-fascinating-stuff
  15. https://www.britannica.com/science/Koppen-climate-classification
  16. https://aa.usno.navy.mil/faq/longest_day
  17. https://kids.britannica.com/students/assembly/view/108060
  18. https://www.thecanadianencyclopedia.ca/en/article/quebec
  19. https://www.britannica.com/place/Greenland
  20. https://www.av8n.com/physics/land-water-latitude.htm
  21. https://www.av8n.com/physics/land-water-latitude.csv
  22. https://www.usgs.gov/faqs/how-much-distance-does-a-degree-minute-and-second-cover-your-maps
  23. https://publications.gc.ca/collections/collection_2011/sen/yc33-0/YC33-0-403-7-eng.pdf
  24. https://www.alamy.com/stock-photo/60-degrees-north-shetland.html
  25. https://confluence.org/confluence.php?lat=60&lon=5
  26. https://latitude.to/articles-by-country/no/norway/190543/sondre-folgefonna
  27. https://latitudelongitude.org/no/bergen/
  28. https://latitudelongitude.org/no/oslo/
  29. https://latitudelongitude.org/se/fagersta/
  30. https://latitude.to/articles-by-country/fi/finland/20200/porkkala
  31. https://latitudelongitude.org/fi/ekenaes/
  32. https://birlinn.co.uk/product/sixty-degrees-north-2/
  33. https://latitude.to/map/ru/russian-federation/cities/kronshtadt
  34. https://latitude.to/map/ru/russian-federation/cities/karpinsk
  35. https://www.britannica.com/place/Ob-River
  36. https://www.britannica.com/place/Lena-River
  37. https://www.britannica.com/science/taiga
  38. https://www.britannica.com/science/tundra-climate
  39. https://collections.dartmouth.edu/arctica-beta/html/EA12-05.html
  40. https://www.alaska.guide/island/kayak-island
  41. https://yukoninfo.com/the-60th-parallel-where-the-north-begins/
  42. https://parks.canada.ca/pn-np/nt/woodbuffalo
  43. https://www.soleica.ca/snowFestival/puvirnituq.html
  44. https://www.shetland.gov.uk/shetland-statistics/physicallocation
  45. https://www.britannica.com/place/Davis-Strait
  46. https://earthobservatory.nasa.gov/images/9033/cape-farewell-greenland
  47. https://www.britannica.com/place/Atlantic-Ocean
  48. https://www.britannica.com/place/Atlantic-Ocean/Hydrology
  49. https://porteconomicsmanagement.org/pemp/contents/part1/interoceanic-passages/main-maritime-shipping-routes/
  50. https://nsidc.org/arcticseaicenews/
  51. https://www.mdpi.com/2077-1312/12/3/517
  52. https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2001JC001214
  53. https://www.usgs.gov/publications/marine-birds-and-mammals-pacific-subarctic-gyres
  54. https://science.nasa.gov/earth/climate-change/historic-low-sea-ice-in-the-bering-sea/
  55. https://nsidc.org/arcticseaicenews/2024/05/
  56. https://nauticalcharts.noaa.gov/publications/coast-pilot/files/cp9/CPB9_C04_WEB.pdf
  57. https://www.fisheries.noaa.gov/alaska/bycatch/frequent-questions-snow-crab-and-salmon-declines-alaska
  58. https://tass.com/russia/702357
  59. https://waves-vagues.dfo-mpo.gc.ca/Library/280328.pdf
  60. https://www.canada.ca/en/environment-climate-change/services/species-risk-public-registry/cosewic-assessments-status-reports/beluga-whale-2020.html
  61. https://www.britannica.com/place/Ungava-Bay
  62. https://www.researchgate.net/publication/227603822_Variability_of_sea_ice_in_Baffin_Bay_and_Davis_Strait
  63. https://panethos.wordpress.com/2016/01/21/worlds-largest-cities-above-60-degrees-north-latitude/
  64. https://www.climate.top/norway/bergen/map/
  65. https://www.latlong.net/place/helsinki-finland-1668.html
  66. https://www.latlong.net/place/st-petersburg-russia-27585.html
  67. https://latitude.to/map/se/sweden/cities/uppsala
  68. https://www.sitesatlas.com/city/CA-Whitehorse/
  69. https://geonames.nrcan.gc.ca/search-place-names/unique?id=LAILN
  70. https://www.geodatos.net/en/coordinates/greenland/narsaq
  71. https://www.worlddata.info/europe/norway/index.php
  72. https://pressbooks.pub/worldgeo/chapter/russia/
  73. https://data.worldbank.org/indicator/EN.POP.DNST?locations=GL
  74. https://data.worldbank.org/indicator/EN.POP.DNST?locations=CA-US
  75. https://www.scb.se/en/finding-statistics/statistics-by-subject-area/population-and-living-conditions/population-composition-and-development/population-statistics/
  76. https://www150.statcan.gc.ca/t1/tbl1/en/tv.action?pid=1710000901
  77. https://www.gov.nu.ca/sites/default/files/documents/2025-06/Nunavut_and_Canada_Population_Estimates_StatsUpdate__First_Quarter_2025.pdf
  78. https://www.statsnwt.ca/population/population-estimates/PopEst_Apr2025.pdf
  79. https://yukon.ca/sites/default/files/2025-07/fin-population-report-q1-2025.pdf
  80. https://stat.gl/beE202505
  81. https://www.internetgeography.net/igcse-geography/population-and-settlement-igcse-geography/what-factors-affect-population-density-and-distribution/
  82. https://publications.gc.ca/collections/collection_2016/bcp-pco/Z1-1991-1-41-50-eng.pdf
  83. https://pure.iiasa.ac.at/id/eprint/14981/1/WP-17-022.pdf
  84. https://www150.statcan.gc.ca/n1/pub/91-520-x/91-520-x2025001-eng.htm
  85. https://www.thearcticinstitute.org/country-backgrounders/canada/
  86. https://60northrun.ca/course/
  87. https://www.worldatlas.com/articles/where-is-the-four-corners-region-of-canada.html
  88. https://laws-lois.justice.gc.ca/eng/acts/N-28.6/page-1.html
  89. https://www.worldatlas.com/maps/russia
  90. https://www.shetland.org/about
  91. https://www.historic-uk.com/HistoryUK/HistoryofScotland/The-History-of-Orkney-Shetland/
  92. https://warfarehistorynetwork.com/article/russias-conquest-of-siberia/
  93. https://arktiskinstitut.dk/fileadmin/files/arktiskinstitut/pdf/01_Why_is_Greenland_a_part_of_the_Danish_kingdom____The_Arctic_Journal.pdf
  94. https://www.shetland.org/blog/norse-influence-shetland-culture
  95. https://www.nps.gov/articles/aredboltfromtheblue.htm
  96. https://alaskahistoricalsociety.org/discover-alaska/glimpses-of-the-past/the-cold-war-years-1946-1991/
  97. https://www.bbc.com/future/article/20250328-why-norway-is-restoring-its-cold-war-military-bunkers
  98. https://aoghs.org/transportation/trans-alaska-pipeline/
  99. https://natural-resources.canada.ca/sites/nrcan/files/CMMP/CMMP_The_Plan-EN.pdf
  100. https://arctic-council.org/about/
  101. https://weatherspark.com/y/52849/Average-Weather-in-Bergen-Norway-Year-Round
  102. https://en.climate-data.org/europe/finland/helsinki/helsinki-5971/
  103. https://weatherspark.com/y/252/Average-Weather-in-Anchorage-Alaska-United-States-Year-Round
  104. https://en.climate-data.org/asia/russian-federation/sakha-republic/yakutsk-1806/
  105. https://en.climate-data.org/europe/norway/hordaland/bergen-100/
  106. https://weatherspark.com/y/91632/Average-Weather-in-Helsinki-Finland-Year-Round
  107. https://en.climate-data.org/north-america/united-states-of-america/alaska/anchorage-1419/
  108. https://weather-and-climate.com/average-monthly-precipitation-Rainfall,nizhnevartovsk-khanty-mansi-okrug-ru,Russia
  109. https://arctic.noaa.gov/report-card/report-card-2022/precipitation/
  110. https://www.climate.gov/news-features/blogs/polar-vortex/polar-vortex-intensifications-overlooked-influencer
  111. https://www.sciencedaily.com/releases/2011/12/111202091148.htm
  112. https://weatherspark.com/y/142848/Average-Weather-in-Yakutsk-Russia-Year-Round
  113. https://weather.com/news/news/earths-coldest-town-siberia-20130123
  114. https://www.amap.no/documents/download/7296/inline
  115. https://climate.copernicus.eu/copernicus-january-2025-was-warmest-record-globally-despite-emerging-la-nina
  116. https://www.sciencedirect.com/science/article/abs/pii/S0921818108001847
  117. https://www.cec.org/files/documents/publications/1701-ecological-regions-north-america-toward-common-perspective-en.pdf
  118. https://www.sciencedirect.com/science/article/pii/S235198942200350X
  119. https://wwfeu.awsassets.panda.org/downloads/russia_forest_cc_final_13nov07.pdf
  120. https://www.pnas.org/doi/10.1073/pnas.1319089111
  121. https://www.hi.no/en/hi/forskning/research-programmes/the-norwegian-sea-ecosystems
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