Kara Sea
Marginal Arctic sea, ice-bound most of the year.
Wikipedia / Wikimedia Commons
The Kara Sea is a marginal sea of the Arctic Ocean, located off the coast of northern Siberia. To the west, it is separated from the Barents Sea by the Kara Strait and the Novaya Zemlya archipelago, while the Severnaya Zemlya archipelago divides it from the Laptev Sea to the east. All three seas are extensions of the Arctic Ocean. The sea stretches roughly 1,450 kilometers (900 miles) in length and 970 kilometers (600 miles) in width, covering an area of about 880,000 square kilometers (339,770 square miles), with an average depth of 110 meters (360 feet). Its northern boundary is defined by a line from Cape Kohlsaat on Graham Bell Island in Franz Josef Land to Cape Molotov (Arctic Cape) on Komsomolets Island in Severnaya Zemlya.
The sea is ice-covered for all but two months of the year, yet it serves as an important fishing ground. Its main ports are Novy Port and Dikson. The Kara Sea holds the East-Prinovozemelsky field, part of the West Siberian Oil Basin, which contains significant but undeveloped reserves of petroleum and natural gas. In 2014, U.S. government sanctions forced Exxon to halt its operations in the sea by September 26.
The sea takes its name from the Kara River, which flows into Baydaratskaya Bay. Though now relatively minor, the river was crucial during the Russian conquest of northern Siberia. The word *kara* likely comes from a Nenets term meaning "hummocked ice," though it may also derive from the Turkic word for "black."
Numerous islands dot the Kara Sea, many of which—such as the Arkticheskiy Institut Islands, Izvesti Tsik Islands, Kirov Islands, Uedineniya (Lonely Island), Wiese Island, and Voronina Island—lie in the open central waters, unlike most Arctic marginal seas where islands cluster near the coast. The largest group is the Nordenskiöld Archipelago, comprising over ninety islands in five subgroups. Other notable islands include Bely Island, Dikson Island, Taymyr Island, the Kamennyye Islands, and Oleni Island. Except for Ushakov Island at the far northern edge, none of the islands are glaciated.
The International Hydrographic Organization defines the sea's limits as follows: on the west, the eastern boundary of the Barents Sea; on the north, from Cape Kohlsaat to Cape Molotov; and on the east, from Komsomolets Island through various capes to Cape Pronchishchev on the mainland. Subareas, listed counterclockwise from west to east, include Baydaratskaya Bay, the Gulf of Ob, the Taz Estuary, Gydan Bay, Yuratski Bay, the Yenisei Gulf, Pyasina Bay, Middendorff Bay, the Taymyr Gulf, Toll Bay, and Zhuravlev Bay on Komsomolets Island. Key straits are the Kara, Kurochkin, Malygina, Matochkin, Red Army, Shokalsky, Taymyr, Vilkitsky, Yugorsky, and Yuny straits.
Water circulation in the Kara Sea is complex and varies by season. The sea is ice-covered from September to May, and from May to August it is heavily influenced by freshwater runoff—roughly 1,200 cubic kilometers per year—from rivers such as the Ob, Yenisei, Pyasina, Pur, and Taz. Inflow from the Barents Sea also plays a role, bringing 0.6 Sverdrups in August and 2.6 Sverdrups in December. This water originates from the Atlantic but cools and mixes with freshwater in the Barents Sea before entering the Kara Sea. Simulations using the Hamburg shelf ocean model (HAMSOM) indicate that no single current pattern persists year-round; currents shift depending on runoff, dominant winds, and sea ice formation.
Historically, the Kara Sea was known as Oceanus Scythicus or Mare Glaciale on 16th-century maps. Ice cover kept it largely unexplored until the late 1800s. In 1556, English explorer Stephen Borough sailed the *Searchthrift* toward the Ob River but was stopped by ice and fog at the sea's entrance. A second English attempt in 1580 by Arthur Pet and Charles Jackman also failed, leading England to abandon the search for a Northeast Passage. In 1736–1737, Russian Admiral Stepan Malygin led an expedition from Dolgy Island in the Barents Sea, commanding the *Perviy* alongside Captain A. Skuratov on the *Vtoroy*. They entered the little-known Kara Sea and reached the Ob River's mouth, making careful observations that allowed Malygin to produce the first reasonably accurate map of the Arctic coast between the Pechora and Ob rivers. In 1878, Finnish explorer Adolf Erik Nordenskiöld sailed the *Vega* from Gothenburg across the Kara Sea and along the Siberian coast, reaching 180° longitude by early September despite ice. The ship wintered in the Chukchi Sea, where Nordenskiöld traded with the local Chukchi people, and was freed the following July, continuing to Yokohama, Japan, as the first to complete the Northeast Passage.
- Area
- around 880,000 km²
- Length
- roughly 1,450 km
- Width
- roughly 970 km
- Mean depth
- 110 metres
- Named after
- Kara river (from Nenets word for 'hummocked ice')
- Main ports
- Novy Port and Dikson
Verified Timeline
Lore & Background
The Kara Sea was formerly known as Oceanus Scythicus or Mare Glaciale and it appears with these names in 16th century maps. Since it is closed by ice most of the year it remained largely unexplored until the late nineteenth century. In 1556 Stephen Borough sailed in the Searchthrift to try to reach the Ob River, but he was stopped by ice and fog at the entrance to the Kara Sea. Not until 1580 did another English expedition, under Arthur Pet and Charles Jackman, attempt its passage. They too failed to penetrate it, and England lost interest in searching for the Northeast Passage. In 1736–1737 Russian Admiral Stepan Malygin undertook a voyage from Dolgy Island in the Barents Sea. The two ships in this early expedition were the Perviy, under Malygin's command and the Vtoroy under Captain A. Skuratov. After entering the little-explored Kara Sea, they sailed to the mouth of the Ob River. Malygin took careful observations of these hitherto almost unknown areas of the Russian Arctic coastline. With this knowledge he was able to draw the first somewhat accurate map of the Arctic shores between the Pechora River and the Ob River. In 1878, Finnish explorer Adolf Erik Nordenskiöld on ship Vega sailed across the Kara Sea from Gothenburg, along the coast of Siberia, and despite the ice packs, got to 180° longitude by early September. Frozen in for the winter in the Chukchi Sea, Nordenskiöld waited and bartered with the local Chukchi people. The following July, the Vega was freed from the ice, and continued to Yokohama, Japan. He became the first to force the Northeast Passage. The year 1912 was a tragic one for Russian explorers in the Kara Sea. In that fateful year unbroken consolidated ice blocked the way for the Northern Sea Route and three expeditions that had to cross the Kara Sea became trapped and failed: Sedov's on vessel St. Foka, Brusilov's on the St. Anna, and Rusanov's on the Gercules. Georgy Sedov intended to reach Franz Josef Land on ship, leave a depot over there, and sledge to the pole. Due to the heavy ice the vessel could only reach Novaya Zemlya the first summer and wintered in Franz Josef Land. In February 1914 Sedov headed to the North Pole with two sailors and three sledges, but he fell ill and died on Rudolf Island. Georgy Brusilov attempted to navigate the Northeast Passage, was trapped in the Kara Sea, and drifted northward for more than two years reaching latitude 83° 17' N. Thirteen men, headed by Valerian Albanov, left the vessel and started across the ice to Franz Josef Land, but only Albanov and one sailor (Alexander Konrad) survived after a gruesome three-month ordeal. The survivors brought the ship log of St. Anna, the map of her drift, and daily meteorological records, but the destiny of those who stayed on board remains unknown. In the same year the expedition of Vladimir Rusanov was lost in the Kara Sea. The prolonged absence of those three expeditions stirred public attention, and a few small rescue expeditions were launched, including Jan Nagórski's five air flights over the sea and ice from the NW coast of Novaya Zemlya. After the Russian Revolution in 1917, the scale and scope of exploration of the Kara Sea increased greatly as part of the work of developing the Northern Sea Route. Polar stations, of which five already existed in 1917, increased in number, providing meteorologic, ice reconnaissance, and radio facilities. By 1932 there were 24 stations, by 1948 about 80, and by the 1970s more than 100. The use of icebreakers and, later, aircraft as platforms for scientific work were developed. In 1929 and 1930 the Icebreaker Sedov carried groups of scientists to Severnaya Zemlya, the last major piece of unsurveyed territory in the Soviet Arctic; the archipelago was completely mapped under Georgy Ushakov between 1930 and 1932. Particularly worth noting are three cruises of the Icebreaker Sadko, which went farther north than most; in 1935 and 1936 the last unexplored areas in the northern Kara Sea were examined and the small and elusive Ushakov Island was discovered. In the summer of 1942, German Kriegsmarine warships and submarines entered the Kara Sea to destroy as many Russian vessels as possible. This naval campaign was named 'Operation Wunderland'. Its success was limited by the presence of ice floes, as well as bad weather and fog. These effectively protected the Soviet ships, preventing the damage that could have been inflicted on the Soviet fleet under fair weather conditions. In October 2010, the Russian government awarded a license to Russian oil company Rosneft for developing the East-Prinovozemelsky oil and gas structure in the Kara Sea.
Reader's Guide
The Kara Sea is roughly 1,450 km long and 970 km wide with an area of around 880,000 km2 and a mean depth of 110 metres. Its main ports are Novy Port and Dikson. The sea is named after the Kara river (flowing into Baydaratskaya Bay), which is now relatively insignificant but which played an important role in the Russian conquest of northern Siberia. The Kara river name is derived from a Nenets word meaning 'hummocked ice'. The International Hydrographic Organization defines the limits of the Kara Sea: on the West, the Eastern limit of Barents Sea; on the North, Cape Kohlsaat to Cape Molotov (81°16′N 93°43′E) (Northern extremity of Severnaya Zemlya on Komsomolets Island); on the East, Komsomolets Island from Cape Molotov to South Eastern Cape, then to Cape Vorochilov, Oktiabrskaya Revolutziya Island to Cape Anuchin, then to Cape Unslicht on Bolshevik Island, Bolshevik Island to Cape Yevgenov, then to Cape Pronchisthehev on the main land. There are many islands and island groups in the Kara Sea. Unlike the other marginal seas of the Arctic, where most islands lie along the coasts, in the Kara Sea many islands, like the Arkticheskiy Institut Islands, the Izvesti Tsik Islands, the Kirov Islands, Uedineniya or Lonely Island, Wiese Island, and Voronina Island are located in the open sea of its central regions. The largest group in the Kara Sea is by far the Nordenskiöld Archipelago, with five large subgroups and over ninety islands. Other important islands in the Kara Sea are Bely Island, Dikson Island, Taymyr Island, the Kamennyye Islands and Oleni Island. Despite the high latitude, all islands are unglaciated except for Ushakov Island at the extreme northern limit of the Kara Sea. Subareas include Baydaratskaya Bay, Gulf of Ob, Taz Estuary, Gydan Bay, Yuratski Bay, Yenisei Gulf, Pyasina Bay, Middendorff Bay, Taymyr Gulf, Toll Bay, and Zhuravlev Bay (Komsomolets Island). Straits include Kara Strait, Kurochkin Strait, Malygina Strait, Matochkin Strait, Red Army Strait, Shokalsky Strait, Taymyr Strait, Vilkitsky Strait, Yugorsky Strait, and Yuny Strait. Water circulation patterns in the Kara Sea are complex. The Kara Sea tends to be sea ice covered between September and May, and between May and August heavily influenced by freshwater run-off (roughly 1200 km3 yr−1) from the Russian rivers (e.g., Ob, Yenisei, Pyasina, Pur, and Taz). The Kara Sea is also affected by the water inflow from the Barents Sea, which brings 0.6 Sv in August and 2.6 Sv in December. The advected water originates from the Atlantic, but it was cooled and mixed with freshwater in the Barents Sea before it reaches the Kara Sea. Simulations with the Hamburg shelf ocean model (HAMSOM) suggest that no typical water current pattern consists in the Kara Sea throughout the year. Depending on the freshwater run-off, the dominant wind patterns, and the sea ice formation, the water currents change. There is concern about radioactive contamination from nuclear waste the former Soviet Union dumped in the sea and the effect this will have on the marine environment. According to an official 'White Paper' report compiled and released by the Russian government in March 1993, the Soviet Union dumped six nuclear submarine reactors and ten nuclear reactors into the Kara Sea between 1965 and 1988. Solid high- and low-level wastes unloaded from Northern Fleet nuclear submarines during reactor refuelings were dumped in the Kara Sea, mainly in the shallow fjords of Novaya Zemlya, where the depths of the dumping sites range from 12 to 135 meters.
Did You Know?
- The Kara Sea is named after the Kara river, whose name comes from a Nenets word meaning 'hummocked ice'.
- In 1736–1737, Russian Admiral Stepan Malygin drew the first somewhat accurate map of the Arctic shores between the Pechora River and the Ob River after sailing into the Kara Sea.
- The year 1912 saw three Russian expeditions become trapped in the Kara Sea: Sedov's on the St. Foka, Brusilov's on the St. Anna, and Rusanov's on the Gercules.
- Between 1965 and 1988, the Soviet Union dumped six nuclear submarine reactors and ten nuclear reactors into the Kara Sea, according to a 1993 Russian government report.
- In 2014, US government sanctions resulted in Exxon having until 26 September to discontinue its operations in the Kara Sea.
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