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Sea of Okhotsk
Sea of Okhotsk
Map of the Sea of Okhotsk
Location	North Asia and East Asia
Coordinates	55°N 150°E / 55°N 150°E / 55; 150
Type	Sea
Basin countries	Japan and Russia
Surface area	1,583,000 km (611,200 sq mi)
Average depth	859 m (2,818 ft)
Max. depth	3,372 m (11,063 ft)

The Sea of Okhotsk is a marginal sea of the western Pacific Ocean. It is located between Russia's Kamchatka Peninsula on the east, the Kuril Islands on the southeast, Japan's island of Hokkaido on the south, the island of Sakhalin along the west, and a stretch of eastern Siberian coast along the west and north. Its northeast corner is the Shelikhov Gulf. The sea is named for the port of Okhotsk, itself named for the Okhota River.

Geography

The Sea of Okhotsk covers an area of 1,583,000 square kilometres (611,000 sq mi), with a mean depth of 859 metres (2,818 ft) and a maximum depth of 3,372 metres (11,063 ft). It is connected to the Sea of Japan on either side of Sakhalin: on the west through the Sakhalin Gulf and the Gulf of Tartary; on the south through the La Pérouse Strait.

In winter, navigation on the Sea of Okhotsk is impeded by ice floes. Ice floes form due to the large amount of freshwater from the Amur River, lowering the salinity of upper levels, often raising the freezing point of the sea surface. The distribution and thickness of ice floes depends on many factors: the location, the time of year, water currents, and the sea temperatures.

Cold air from Siberia forms sea ice in the northwestern Sea of Okhotsk. As the ice forms, it expels salt into the deeper layers. This heavy water flows east toward the Pacific, carrying oxygen and nutrients, supporting abundant sea life. The Sea of Okhotsk has warmed in some places by as much as 3°C (5.4°F) since preindustrial times, three times faster than the global mean. Warming inhibits the formation of sea ice and also drives fish populations north. The salmon catch on the northern Japanese coast has fallen 70% in the last 15 years, while the Russian chum salmon catch has quadrupled.

With the exception of Hokkaido, one of the Japanese home islands, the sea is surrounded on all sides by territory administered by the Russian Federation. South Sakhalin and the Kuril Islands were administered by Japan until 1945. Japan claims the southern Kuril Islands and refers to them as Northern Territories.

• Gallery
• Nagayevo Bay near Magadan, Russia
• Shiretoko National Park on the Sea of Okhotsk coast of Hokkaido, Japan

Extent

The International Hydrographic Organization defines the limits of the Sea of Okhotsk as follows:

::On the Southwest. The Northeastern and Northern limits on the Japan Sea .

::On the Southeast. A line running from Nosyappu Saki (Cape Noshap, 43°23'N) in the Island of Hokusyû (Yezo) through the Kuril or Tisima Islands to Cape Lopatka (South point of Kamchatka) in such a way that all the narrow waters between Hokusyû and Kamchatka are included in the Sea of Okhotsk.

Islands

Some of the Sea of Okhotsk's islands are quite large, including Japan's second-largest island, Hokkaido, as well as Russia's largest island, Sakhalin. Practically all of the sea's islands are either in coastal waters or belong to the various islands making up the Kuril Islands chain. These fall either under undisputed Japanese or Russian ownership or disputed ownership between Japan and Russia. Iony Island is the only island located in open waters and belongs to the Khabarovsk Krai of the Russian Federation.

The majority of the sea's islands are uninhabited, making them ideal breeding grounds for seals, sea lions, seabirds, and other sea island fauna. Large colonies of crested auklets use the Sea of Okhotsk as a nesting site.

History

Pre-modern

The Okhotsk culture and the later Ainu people, a coastal fishing and hunter-gatherer people, were located around the lands surrounding the Sea of Okhotsk, as well as in northern Japan.

European exploration and settlement

Russian explorers Vassili Poyarkov(1639) and Ivan Moskvitin (1645) were the first Europeans to visit the Sea of Okhotsk (and, probably, the island of Sakhalin) in the 1640s. The Dutch captain Maarten Gerritsz Vries in the Breskens entered the Sea of Okhotsk from the south-east in 1643, and charted parts of the Sakhalin coast and Kuril Islands, but failed to realize that either Sakhalin or Hokkaido are islands. During this period, the sea was sometimes known as the Sea of Kamchatka.

The first and foremost Russian settlement on the shore was the port of Okhotsk, which relinquished commercial supremacy to Ayan in the 1840s. The Russian-American Company all but monopolized the commercial navigation of the sea in the first half of the 19th century.

The Second Kamchatka Expedition under Vitus Bering systematically mapped the entire coast of the sea, starting in 1733. Jean-François de Galaup, comte de Lapérouse and William Robert Broughton were the first non-Russian European navigators known to have passed through these waters other than Vries. Ivan Krusenstern explored the eastern coast of Sakhalin in 1805. Mamiya Rinzō and Gennady Nevelskoy determined that Sakhalin was indeed an island separated from the mainland by a narrow strait. The first detailed summary of the hydrology of the Sea of Okhotsk was prepared and published by Stepan Makarov in 1894.

Fishing

The Sea of Okhotsk is rich in biological resources, with various kinds of fish, shellfish and crabs.

The harsh conditions of crab fishing in the Sea of Okhotsk is the subject of the most famous novel of the Japanese writer Takiji Kobayashi, The Crab Cannery Ship (1929).

The Peanut Hole

The Peanut Hole (named for its shape) was an area of open ocean at the center of the Sea of Okhotsk, about 55 km (30 mi) wide and 480 km (300 mi) long, that was surrounded by Russia's exclusive economic zone (EEZ). Since the Peanut Hole was not in the Russian EEZ, any country could fish there, and some began doing so in large numbers in 1991, catching perhaps as much as one million metric tons of pollock in 1992. This was seen by the Russian Federation as presenting a danger to Russian fish stocks, since the fish move in and out of the Peanut Hole from the Russian EEZ.

The Russian Federation petitioned the United Nations to declare the Peanut Hole to be part of Russia's continental shelf. In November 2013, a United Nations subcommittee accepted the Russian argument, and in March 2014 the full United Nations Commission on the Limits of the Continental Shelf ruled in favor of the Russian Federation.

Whaling

Bowhead whales were first caught in 1847, and dominated the catch between 1852 and the late 1860s. Between 1850 and 1853 the majority of the fleet went to the Bering Strait region to hunt bowheads, but intense competition, poor ice conditions, and declining catches forced the fleet back to the Sea of Okhotsk. From 1854 to 1856, an average of over 160 vessels cruised in the sea each year. As catches declined between 1858 and 1860 the fleet shifted back to the Bering Strait region.

The Russian military marine mammal program reportedly sources some of its animals from the Sea of Okhotsk.

Modern

South Sakhalin was administered by Japan as Karafuto Prefecture from 1907 to 1949. The Kuril Islands were Japanese from 1855 and 1875 till the end of World War II in 1945. Afterward, the Soviet Union occupied the territory.

During the Cold War, the Sea of Okhotsk was the scene of several successful U.S. Navy operations (including Operation Ivy Bells) to tap Soviet Navy undersea communications cables. These operations were documented in the 1998 book Blind Man's Bluff: The Untold Story of American Submarine Espionage. The sea (and surrounding area) were also the scene of the Soviet attack on Korean Air Lines Flight 007 in 1983. The Soviet Pacific Fleet used the sea as a ballistic missile submarine bastion, a strategy that Russia continues.

Despite its proximity to Japan, the Sea of Okhotsk has no native etymology in the Japanese language; its name, Ohōtsuku-kai (オホーツク海), is a transcription of the Russian name. This is also reflected in the name of Hokkaidō's Okhotsk Subprefecture, which faces the Sea of Okhotsk and is also known as the Okhotsk region (オホーツク地方, Ohōtsuku-chihō).

Oil and gas exploration

Twenty-nine zones of possible oil and gas accumulation have been identified on the Sea of Okhotsk shelf, which runs along the coast. Total reserves are estimated at 3.5 billion tons of equivalent fuel, including 1.2 billion tons of oil and 1.5 billion cubic meters of gas.

On 18 December 2011, the Russian oil drilling rig Kolskaya capsized and sank in a storm in the Sea of Okhotsk, some 124 km (77 mi) from Sakhalin island, where it was being towed from Kamchatka. Reportedly, its pumps failed, causing it to take on water and sink. The platform carried 67 people, of which 14 were rescued by the Magadan and the tugboat Natftogaz-55. The platform was subcontracted to a company working for the Russian energy giant Gazprom.

Notable seaports

• Magadan, Magadan, Russia; population: 95,000
• Palana, Kamchatka, Russia; population: 3,000
• Abashiri, Hokkaido, Japan; population: 38,000
• Monbetsu, Hokkaido, Japan; population: 25,000
• Wakkanai, Hokkaido, Japan; population: 38,000

See also

• 100 Soundscapes of Japan
• History of fur trade by Sea of Okhotsk

Explanatory notes

1. Russian: Охотское море, romanized: Okhotskoye more, IPA: [ɐˈxotskəjə ˈmorʲe]; Historically also known as Ламутское море, Lamutskoye more, or as Камчатское море, Kamchatskoye more; Japanese: オホーツク海, romanized: Ohōtsuku-kai)

References

1. Kon-Kee Liu; Larry Atkinson (June 2009). Carbon and Nutrient Fluxes in Continental Margins: A Global Synthesis. Springer. pp. 331–333. ISBN 978-3-540-92734-1. Retrieved 29 November 2010.
2. Everett-Heath, John (2020). "Okhotsk, Sea of (Okhotskoye More)". Concise Oxford Dictionary of World Place Names (6th ed.). Oxford University Press. ISBN 9780191905636.
3. "Sea of Okhotsk - Economic aspects". Encyclopedia Britannica. Retrieved 2019-11-14.
4. Watanabe, Tatsuro; Ikeda, Motoyoshi; Wakatsuchi, Masaaki (2004). "Thermohaline effects of the seasonal sea ice cover in the Sea of Okhotsk". Journal of Geophysical Research: Oceans. 109 (C9). Bibcode:2004JGRC..109.9S02W. doi:10.1029/2003JC001905. ISSN 2156-2202.
5. "How climate change is triggering a chain reaction that threatens the heart of the Pacific". Washington Post. Retrieved 2019-11-14.. Print 15nov19, pp A1, A12, A13.
6. Bruce A. Elleman, Michael R. Nichols and Matthew J. Ouimet, A Historical Reevaluation of America's Role in the Kuril Islands Dispute, Pacific Affairs, Vol. 71, No. 4 (Winter, 1998–1999), pp. 489–504
7. "Limits of Oceans and Seas" (PDF). Nature. 172 (4376) (3rd ed.). International Hydrographic Organization: 32–33. 1953. Bibcode:1953Natur.172R.484.. doi:10.1038/172484b0. S2CID 36029611. Retrieved 15 June 2020.
8. "ウェブマガジン カムイミンタラ ～北海道の風土・文化誌 ：オホーツク文化人とモヨロ貝塚 網走 流氷とともにやってきた古代民族の謎とロマンに魅せられた父子三代と研究者たち" ["Web Magazine Kamuy Mintara ~Hokkaido's Climate and Culture Magazine: Okhotsk Culture and Moyoro Shell Mounds Abashiri Three generations of fathers and sons and researchers fascinated by the mystery and romance of ancient peoples who came along with the drift ice".]. kamuimintara.net. Retrieved 2019-07-10.
9. Pavel Ushakov [ru], Sea of Okhotsk, In: Морской сборник, Issue 1, 1940, pp.69-92
10. Stephan, John J. (1971), Sakhalin: a history, Clarendon Press, p. 11
11. "Plate LXXXVII. Fig. 2. World.", Encyclopaedia Britannica, vol. II (1st ed.), Edinburgh: Colin Macfarquhar, 1771.
12. Vaughan, R. (1984). "Historical survey of the European whaling industry". In Arctic Whaling: Proceedings of the International Symposium, pp. 121-145. University of Groningen.
13. Bockstoce, John (1986). Whales, Ice, & Men: The History of Whaling in the Western Arctic. University of Washington Press. ISBN 0-295-97447-8.
14. Jabr, Ferris (2024-01-04). "The Whale Who Went AWOL". New York Times.
15. Acharya, Amitav (March 1988). "The United States Versus the USSR in the Pacific: Trends in the Military Balance". Contemporary Southeast Asia. 9 (4). Institute of Southeast Asian Studies: 293. ISSN 1793-284X. JSTOR 25797972.
16. "Magadan Region". Kommersant, Russia's Daily Online. Archived from the original on October 25, 2007. Retrieved January 22, 2007.
17. Technical details of the rig www.amngr.ru
18. "Rig Data: Kolskaya". Rigzone. Archived from the original on 2012-01-03. Retrieved 2011-12-19.
19. "Russian oil rig sinks, leaving many missing". CNN. December 18, 2011. Retrieved December 18, 2011.
20. "Kolskaya Sinks Offshore Russia". Rigzone. Retrieved August 13, 2012.
21. "Blog Archive » Rig Kolskaya Lost". Shipwreck Log. December 18, 2011. Retrieved August 13, 2012.

External links

• Overview of Okhotsk region (PDF) Archived 2012-02-07 at the Wayback Machine

v t e Islands of the Sea of Okhotsk

Antsiferov Atlasov Banka Zotova Baydukov and Belyakov Belichy Bolshoy Chome Bolshoy Shantar Broutona Chastye Islands Chetyre Paltsa Chirinkotan Chkalov Chyornye Bratya (Chirpoy and Brat Chirpoyev) Dobrzhansky Ekarma Feklistova Glinyanyy Hokkaido Iony Iturup Ivyinichaman Kamen-Mukdykyn Kamen Opasnosti Kekurny Ketoy Khalpili Islands Kharimkotan Konus Kunashir Kuril Islands Kusova Makanrushi Maly Shantar Matua Medvezhy Menshikov Morskaya Matuga Nansikan Nedorazumeniya Onekotan Oremif Paramushir Pilamif Prokofyeva Ptichy Island (Kamchatka Krai) Ptichy Island (Shantar Islands) Raikoke Rasshua Rechnaya Matuga Reyneke Rovny Island Sakhalin Sakharnaya Golova Shantar Islands Shelikan Shiashkotan Shumshu Simushir Sivuch'i Rocks Spafaryev, Ryabokon and Talan Telan Trety, Krayny and Vtoroy Tyuleny Umara Urup Ush Ushishir Utichy Yam Islands Yengalychev Zavyalov Zubchaty

• Sea of Okhotsk
• Bodies of water of Kamchatka Krai
• Bodies of water of Khabarovsk Krai
• Bodies of water of Magadan Oblast
• Bodies of water of Sakhalin Oblast
• Geography of Hokkaido
• Geography of Northeast Asia
• Geography of the Russian Far East
• Marginal seas of the Pacific Ocean
• Pacific Coast of Russia
• Seas of Asia
• Seas of Japan
• Seas of Russia
• Temperate Northern Pacific