This sea is one of the least studied in the Arctic area. It is characterized by severeclimate, low watersalinity, and a scarcity of flora, fauna and human population, as well as shallow depths (mostly less than 50 m), slowsea currents, lowtides (below 25 cm), frequentfogs, especially in summer, and an abundance ofice fields which fully melt only in August–September. The sea shores were inhabited for thousands of years[citation needed] by indigenous tribes ofYukaghirs,Chukchi and thenEvens andEvenks, which were engaged in fishing, hunting andreindeer husbandry. They were then absorbed byYakuts and later byRussians.
Major industrial activities in the area are mining and navigation within theNorthern Sea Route; commercial fishing is poorly developed. The largest city and port[5] isPevek, thenorthernmost city of mainland Russia.[6][7][8]
The present name was assigned to the sea on 27 June 1935 by Decree of the Soviet Government. Before that, the sea had no distinct name, and a variety of names were interchangeably used to refer to it in Russia, includingIndigirskoe,Kolymskoe,Severnoe (Northern),Sibirskoe andLedovitoe (Icy).[9]
On the West. The Eastern limit ofLaptev Sea [From the Northern extremity ofKotelni Island – through Kotelni Island to Cape Madvejyi. Then throughMalyi Island, to Cape Vaguin onGreat Liakhov Island. Thence to Cape Sviaroy Noss on the main land].
Satellite photo of the New Siberian Islands, with the Laptev Sea on the left and part of the East Siberian Sea shown on the right.
Because it is open towards the Arctic Ocean in the north, the main gulfs of the East Siberian Sea, like theKolyma Bay, theKolyma Gulf and theChaunskaya Bay, are all located in its southern limits. There are no islands in the middle of the East Siberian Sea, but there are a few islands and island groups in its coastal waters, likeAyon Island and theMedvyezhi island group. The total area of the islands is only 80 km2.[11] Some islands mostly consist of sand and ice and gradually erode.[2]
The total catchment area is 1,342,000 km2.[12] Among the rivers flowing into the East Siberian Sea, theIndigirka,Alazeya,Chukochya,Kolyma,Rauchua,Chaun, andPegtymel are the most important. Only a few rivers are navigable.[13] The coastline of the sea is 3,016 km long.[11] It makes large bends, sometimes stretching deep into the land, and has a rather different topography in the eastern and western parts. Fine bends are rare and occur only in the riverdeltas. The coastal section between the New Siberian Islands and the mouth of the Kolyma River is uniform, with low and slowly varying slopes. It extends landwards to the marshytundra filled with numerous small lakes. In contrast, the coast to the east of the Kolyma River is mountainous, with steep cliffs.[2][4]
The underwater topography of the shelf that forms the seabed is a plain, sloping from southwest to northeast, covered in a mixture of silt, sand and stones and lacking significant depressions and elevations. About 70% of the sea is shallower than 50 m, with predominant depths of 20–25 m. North-east to the mouth of the Kolyma and Indigirka rivers, there are deep trenches on the seabed, which are attributed to the ancient river valleys, now submerged by the sea. The region of small depths in the western part forms the Novosibirsk shoal. The greatest depths of about 915 m are found in the north-eastern part of the sea.[2][4][14]
The East Siberian Sea is bound to the south by theEast Siberian Lowland, an alluvial plain mainly composed of sediments of marine origin dating back to the time when the whole area was occupied by theVerkhoyansk Sea, an ancient sea at the edge of theSiberian Craton in thePermian period. As centuries went by, gradually, most of the area limiting the sea, as well as the contiguous Laptev Sea to the south became filled with the alluvial deposits of modern rivers.[15]
The climate is polar and is influenced by the continent and Atlantic and Pacific oceans. In winter, it is mostly affected by the continent. South-westerly and southerly winds having the speeds of 6–7 m/s (15 mph, 25 km/h) bring cold air from Siberia, so the average temperature in January is approximately −30 °C. The weather is calm, clear and stable with occasional intrusions by cyclones. Atlantic cyclones increase the wind speed and air temperature whereas Pacific ones bring clouds, storms and blizzards.
The winds blow from the north in summer; they are weak in June, strengthen to 6–7 m/s (15 mph, 25 km/h) in July and reach 10–15 m/s (33 mph, 50 km/h) in August, making the western part of the sea one of the most violent areas on the northern Russian coast. The southeastern part is however much calmer. Northerly winds result in the low average temperatures of 0–1 °C in the open sea and 2–3 °C on the coast in July. Skies are usually cloudy, with frequent drizzling rains or wet snow.[4] Along the coasts, fogs occur 90–100 days per year, mostly in summer (68–75 days).[13][14] Precipitation is low at 100–200 mm per year,[2] but it is still larger than the evaporation volume.[11]
Ice in the East Siberian SeaSea ice retreat in the East Siberian Sea. Top: 15 June 2007, bottom: 27 July the same year.[16]
The continental runoff into the East Siberian Sea is relatively small at about 250 km3/year that makes only 10% of the total runoff in all the Arctic seas of Russia. The largest contribution is from the Kolyma River at 132 km3, followed by the Indigirka River at 59 km3. Most runoff (90%) occurs in summer; it is concentrated near the coast, owing to the weak river currents, and therefore does not significantly affect the sea hydrology.[4] The water exchange between the neighboring seas is as follows. The annual outflow to the Laptev Sea, Chukchi Sea and Arctic Ocean is 3,240, 6,600 and 11,430 km3, respectively; while the respective inflow values are 3,240, 8,800 and 9,230 km3.[11]
The surface water temperature decreases from south to north. In winter it varies between −0.2 and 0.6 °C at the river deltas and from −1.7 to −1.8 °C in the northern sea part. In summer, it warms to 7–8 °C in the bays and inlets and to 2–3 °C in the ice-free sea zones.[4]
Surface water salinity increases from southwest to northeast. In winter and spring, it is 4–5‰ (parts per thousand) near the deltas of the Kolyma and Indigirka rivers. It increases to 28–30‰ in the sea centre, reaching 31–32‰ at its northern outskirts. Salinity decreases in summer by some 5‰ due to the snow melting. It also decreases by some 5–7‰ from the sea bottom to the surface.[4]
There are constant currents at the sea surface directed from west to east. They are weak and thus can temporarily change direction due to the wind. Thetides are semidiurnal (rising twice a day) with the amplitude between 5 and 25 cm. The tidal wave weakens toward the coast due to shallow waters. The sea level is maximal in summer, due to the river runoff, and in autumn due to the winds. It is the lowest in March–April, with the total annual fluctuations within about 70 cm. Winds bring storms with waves reaching 3–5 m in the western part whereas the eastern regions are relatively calm.[4] The storms typically last 1–2 days in summer; they are more frequent in winter and may extend up to 3–5 days.[13]
The sea freezes over between October–November and June–July. The ice is continuous and stationary near the coast, reaching the thickness of 2 m by the end of winter; The thickness decreases from west to east. Further into the sea, the ice cover transforms into drifting ice having the thickness of 2–3 m. The southern winter winds shift this ice northwards, makingpolynyas near the sea centre.[4] There are noicebergs in the sea. Ice melting typically starts around May, first around the delta of the major Kolyma River.[13]
In absence of industry, sea water is rather clean. Minor contaminations are found near the Novosibirsk and Wrangel islands (up to 80 μg/L), due to occasional oil spills,[12] and in Chaunskaya Bay due to the localthermal power station and activities at the major port Pevek.[17][18]
Flora and fauna are relatively scarce due to the harsh climate. The summerplankton bloom is short but intense, producing 5 million tonnes of plankton in August and September, whereas the annual production is 7 million tonnes. The nutrients in water are mostly provided by river discharges andcoastal erosion. The plankton species are dominated by the Pacific species ofcopepods.[12]
The coast of the East Siberian Sea was inhabited for ages by the native peoples of northern Siberia such asYukaghirs andChukchi (eastern areas). Those tribes were engaged in fishing, hunting andreindeer husbandry, as reindeer sleds were essential for transportation and hunting. They were joined and absorbed byEvens andEvenks around the second century and later, between ninth and 15th centuries, by much more numerousYakuts. All those tribes moved north from theBaikal Lake area avoiding confrontations with Mongols. Whereas they all practisedshamanism, they spoke different languages.[20][21][22][23]
The sea was navigated by Russian sea-farers, moving from one river mouth to another in theirkochs as early as the 17th century. In 1648,Semyon Dezhnev andFedot Alekseev sailed the coast of the East Siberian Sea from the Kolyma to riverAnadyr in theBering Sea. Systematic exploration and mapping of the sea and its coasts was carried out by a series of expeditions in1735–42, 1820–24, 1822, 1909 and 1911–14.[2]
In the 1930s, the coastal settlement ofAmbarchik, located at the delta of the Kolyma River, was used as a transientlabor camp from which prisoners were transported to other northern camps of theGulag system. While stationed at Ambarchik, prisoners were employed to build most of the port infrastructure and to unload the incoming ships. Later, due to shallow waters, the shipping was gradually transferred toChersky in the lower reaches of the Kolyma, in order to accommodate larger vessels. As a result of this transfer, the port and settlement have been abandoned. Nowadays, Ambarchik only hosts a meteorological station operated by a few staff members.[24]
Another two labour camps of the Gulag system were later opened near Pevek, namely Chaunlag (1951–1953) and Chaunchukotlag (1949–1957). Both contained about 10,000 inmates used in the mine and construction works.[25][26]
The southern coast of the sea is shared by theSakha Republic on the west andChukotka Autonomous Okrug of Russia on the east. The coastal settlements are few and small, with the typical population below 100. The only city isPevek (population 5,206), which is thenorthernmost city in Russia. There are gold mines nearLeningradsky and Pevek, but many mines have been closed recently, for example,tin mines at Pevek in the 1990s, that resulted in outflow of population.[27] So, theLogashkino settlement, which used to be a notable East Siberian Sea port, was abolished in 1998.[28]
The sea is used mostly for transportation of goods across the northern coast of Russia during August–September. The navigation is hindered even in summer by the remaining floating ice which is also brought down to the southern shores by occasional winds.[13] Fishery and hunting of marine animals is still practised as traditional activities, but has only local importance.[4] Fishery mostly targets salmon, halibut and crab. Data exist on fish production, which in 2005 was distributed, in thousand tonnes as follows:sardine (1.6),Arctic cisco (1.8),Bering cisco (2.2),broad whitefish (2.7),Muksun (2.8) and others (3.6).[12]
The principal port isPevek (in the Chaunskaya Bay)[29] After the breakup of theSoviet Union, commercial navigation in the Arctic went into decline. Nowadays more or less regular shipping occurs only between Pevek andVladivostok. Ports in the northern Siberian coast located betweenDudinka and Pevek see next to no shipping at all.
Since 1944, most electricity for the region is provided by the 30 MWthermal power station of Pevek. It is ageing and consumes much oil which has to be brought from far away. Therefore, there was a project to replace the station by a floating 70 MW atomic power station by 2015. (failed)[30]
^"East Siberian Sea". Archived from the original on September 19, 2010. Retrieved2010-09-12.{{cite web}}: CS1 maint: bot: original URL status unknown (link).rospriroda.ru (in Russian)
^Resolution #443 of September 29, 1998On Exclusion of Inhabited Localities from the Records of Administrative and Territorial Division of the Sakha (Yakutia) Republic
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