Баренцево море: География, климат и история

Marginal sea of the Arctic Ocean, off the northern coasts of Norway and Russia

The Barents Sea ('/b//ær//ə//n//t//s/ BARRənts, also /US/'/b//ɑːr//ə//n//t//s/ BARənts; Barentshavet, ; Баренцево море) is a marginal sea of the Arctic Ocean, located off the northern coasts of Norway and Russia and divided between Norwegian and Russian territorial waters. It was known earlier among Russians as the Northern Sea, Pomorsky Sea or Murman Sea ("Norse Sea"); the current name of the sea is after the historical Dutch navigator Willem Barentsz. The Barents Sea is a rather shallow shelf sea with an average depth of , and it is an important site for both fishing and hydrocarbon exploration. It is bordered by the Kola Peninsula to the south, the shelf edge towards the Norwegian Sea to the west, the archipelagos of Svalbard to the northwest, Franz Josef Land to the northeast and Novaya Zemlya to the east. The islands of Novaya Zemlya, an extension of the northern end of the Ural Mountains, separate the Barents Sea from the Kara Sea. Although part of the Arctic Ocean, the Barents Sea has been characterised as "turning into the Atlantic" One prediction is that, as the Barents Sea's permanent ice free area grows, evaporation will increase, leading to increased winter snowfalls in much of continental Europe.

The southern half of the Barents Sea, including the ports of Murmansk (Russia) and Vardø (Norway) remain ice free year round due to the warm North Atlantic drift. In September, the entire Barents Sea is more or less completely ice free. In 1944, Finland's territory also reached the Barents Sea. The Liinakhamari harbour in the Pechengsky District was Finland's only ice free winter harbour until it was ceded to the Soviet Union. There are three main types of water masses in the Barents Sea: Warm, salty Atlantic water (temperature >3 °C, salinity >35) from the North Atlantic drift; cold Arctic water (temperature <0 °C, salinity <35) from the north; and warm, but not very salty, coastal water (temperature >3 °C, salinity <34.7). Between the Atlantic and Polar waters, a front called the Polar Front is formed. In the western parts of the sea (close to Bear Island), this front is determined by the bottom topography and is therefore relatively sharp and stable from year to year, while in the east (towards Novaya Zemlya), it can be quite diffuse and its position can vary markedly between years. The lands of Novaya Zemlya attained most of their early Holocene coastal deglaciation approximately 10,000 years before the present.

The Barents Sea was originally formed from two major continental collisions: the Caledonian orogeny, in which the Baltica and Laurentia collided to form Laurasia, and a subsequent collision between Laurasia and Western Siberia. Most of its geological history is dominated by extensional tectonics, caused by the collapse of the Caledonian and Uralian orogenic belts and the break up of Pangaea. These events created the major rift basins that dominate the Barents Shelf, along with various platforms and structural highs. The later geological history of the Barents Sea is dominated by Late Cenozoic uplift, particularly that caused by Quaternary glaciation, which has resulted in erosion and deposition of significant sediment.

Due to the North Atlantic drift, the Barents Sea has a high biological production compared to other oceans of similar latitude. The spring bloom of phytoplankton can start quite early near the ice edge because the fresh water from the melting ice makes up a stable water layer on top of the seawater. The phytoplankton bloom feeds zooplankton such as Calanus finmarchicus, Calanus glacialis, Calanus hyperboreus, Oithona spp., and krill. The zooplankton feeders include young cod, capelin, polar cod, whales, and little auk. The capelin is a key food for top predators such as the north east Arctic cod, harp seals, and seabirds such as the common guillemot and Brunnich's guillemot. The fisheries of the Barents Sea, in particular the cod fisheries, are of great importance for both Norway and Russia. SIZEX 89 was an international winter experiment in 1989 for which the main objectives were to perform sensor signature studies of different ice types to develop SAR algorithms for ice variables, such as ice types, ice concentrations and ice kinematics. Although previous research suggested that predation by whales may be the cause of depleting fish stocks, more recent research suggests that marine mammal consumption has only a trivial influence on fisheries. A model assessing the effects of fisheries and climate was far more accurate at describing trends in fish abundance. There is a genetically distinct polar bear population associated with the Barents Sea.

The Barents Sea is "among the most polluted places on Earth" due to accumulated marine garbage, decades of Soviet nuclear tests, radioactive waste dumping and industrial pollution. The elevated pollution has caused elevated rates of disease among locals. This sea was given its present name by Europeans in honour of Willem Barentsz, a Dutch navigator and explorer. Barentsz was the leader of early expeditions to the far north, at the end of the sixteenth century. The Barents Sea has been called by sailors "The Devil's Dance Floor" due to its unpredictability and difficulty level. Ocean rowers call it "Devil's Jaw". In 2017, after the first recorded complete man powered crossing of the Barents Sea from Tromsø to Longyearbyen in a rowboat by the Polar Row expedition, captain Fiann Paul was asked by Norwegian TV2 how a rower would name the Barents Sea. Fiann responded that he would name it "Devil's Jaw", adding that the winds you constantly battle are like breath from the devil's nostrils while he holds you in his jaws.

Seabed mapping was completed in 1933; the first full map was produced by Russian marine geologist Maria Klenova. The Barents Sea was the site of a notable World War II engagement which later became known as the Battle of the Barents Sea. Under the command of Oskar Kummetz, German warships sank minelayer HMS Bramble and destroyer but lost destroyer German destroyer Z16 Friedrich Eckoldt. Also, the German cruiser German cruiser Admiral Hipper was severely damaged by British gunfire. The Germans later retreated and the British convoy arrived safely at Murmansk shortly afterwards. During the Cold War, the Soviet Red Banner Northern Fleet used the southern reaches of the sea as a ballistic missile submarine bastion, a strategy that Russia continued. Nuclear contamination from dumped Russian naval reactors is an environmental concern in the Barents Sea.

For decades there was a boundary dispute between Norway and Russia regarding the position of the boundary between their respective claims to the Barents Sea. The Norwegians favoured a median line, based on the Geneva Convention of 1958, whereas the Russians favoured a meridian based sector line, based on a Soviet decision of 1926.

Encouraged by the success of oil exploration and production in the North Sea in the 1960s, Norway began hydrocarbon exploration in the Barents Sea in 1969. They acquired seismic reflection surveys through the following years, which were analysed to understand the location of the main sedimentary basins. However, interest in the area began to wane due to a succession of dry holes, wells containing only gas (which was cheap at the time), and the prohibitive costs of developing wells in such a remote area. Interest in the area was reignited in the late 2000s after the Snovhit field was finally brought into production and two new large discoveries were made. The Russians began exploration in their territory around the same time, encouraged by their success in the Timan Pechora Basin. as well as important stocks of haddock and capelin. Fishing is managed jointly by Russia and Norway in the form of the Joint Norwegian–Russian Fisheries Commission, established in 1976, in an attempt to keep track of how many fish are leaving the ecosystem due to fishing. The Joint Norwegian Russian Fisheries Commission sets Total Allowable Catches (TACs) for multiple species throughout their migratory tracks. Through the Commission, Norway and Russia also exchange fishing quotas and catch statistics to ensure the TACs are not being violated. However there are problems with reporting under this system, and researchers believe that they do not have accurate data for the effects of fishing on the Barents Sea ecosystem. Cod is one of the major catches. A large portion of catches are not reported when the fishing boats land, to account for profits that are being lost to high taxes and fees. Since many fishermen do not strictly follow the TACs and rules set forth by the Commission, the amount of fish being extracted annually from the Barents Sea is underestimated.

The Barents Sea, where temperate waters from the Gulf Stream and cold waters from the Arctic meet, is home to an enormous diversity of organisms, which are well adapted to the extreme conditions of their marine habitats. This makes these arctic species very attractive for marine bioprospecting. Marine bioprospecting may be defined as the search for bioactive molecules and compounds from marine sources that have new, unique properties and the potential for commercial applications. Amongst others, applications include medicines, food and feed, textiles, cosmetics and the process industry. The Norwegian government strategically supports the development of marine bioprospecting as it has the potential to contribute to new and sustainable wealth creation. Tromsø and the northern areas of Norway play a central role in this strategy. They have excellent access to unique Arctic marine organisms, existing marine industries, and R&D competence and infrastructure in this region. Since 2007, science and industry have cooperated closely on bioprospecting and the development and commercialization of new products.