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Geography

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.