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  2. Atlantification of the Arctic - Wikipedia

    en.wikipedia.org/wiki/Atlantification_of_the_Arctic

    Sea surface temperature difference between the decades 1960-1970 and 2010-2020 in degrees C. [1] Location of the Barents Sea in the Arctic Ocean. Atlantification is the increasing influence of Atlantic water in the Arctic. Warmer and saltier Atlantic water is extending its reach northward into the Arctic Ocean. [2]

  3. Arctic dipole anomaly - Wikipedia

    en.wikipedia.org/wiki/Arctic_dipole_anomaly

    Wang et al. [14] suggest that in addition to anomalous winds driving sea ice out of the Arctic through the Fram Strait, the positive phase of the Arctic dipole anomalies may also increase the flow of relatively warm waters from the North Pacific through the Bering Strait into the Arctic Ocean. Warmer waters, in addition to increased sea ice ...

  4. Barents Sea - Wikipedia

    en.wikipedia.org/wiki/Barents_Sea

    The Barents Sea (/ ˈ b ær ə n t s / BARR-ənts, also US: / ˈ b ɑːr ə n t s / BAR-ənts; [1] Norwegian: Barentshavet, Urban East Norwegian: [ˈbɑ̀ːrəntsˌhɑːvə]; [2] Russian: Баренцево море, romanized: Barentsevo More) is a marginal sea of the Arctic Ocean, [3] located off the northern coasts of Norway and Russia and divided between Norwegian and Russian territorial ...

  5. The Arctic Ocean could be 'ice-free' within the decade ... - AOL

    www.aol.com/news/arctic-ocean-could-ice-free...

    The first ice-free days of the Arctic Ocean could occur as soon as the 2020s or 2030s — as many as 10 years earlier than previous projections.

  6. Arctic Ocean - Wikipedia

    en.wikipedia.org/wiki/Arctic_Ocean

    The Arctic Ocean is the smallest and shallowest of the world's five oceanic divisions. [1] It spans an area of approximately 14,060,000 km 2 (5,430,000 sq mi) and is the coldest of the world's oceans.

  7. Kara Sea - Wikipedia

    en.wikipedia.org/wiki/Kara_Sea

    Ultimately the Kara, Barents and Laptev Seas are all extensions of the Arctic Ocean north of Siberia. The Kara Sea's northern limit is marked geographically by a line running from Cape Kohlsaat in Graham Bell Island, Franz Josef Land, to Cape Molotov (Arctic Cape), the northernmost point of Komsomolets Island in Severnaya Zemlya.

  8. Arctic ocean may absorb less CO2 than projected due to ... - AOL

    www.aol.com/news/planet-warms-arctic-ocean...

    The Arctic Ocean's ability to absorb carbon dioxide from the atmosphere appears to be waning due to melting permafrost and worsening coastal erosion.

  9. Fram Strait - Wikipedia

    en.wikipedia.org/wiki/Fram_Strait

    The warming in the Fram Strait region has likely amplified Arctic shrinkage, and serves as a positive feedback mechanism for transporting more internal energy to the Arctic Ocean. [ 15 ] In the past century, the sea surface temperature at Fram Strait has on average warmed roughly 1.9 °C (3.5 °F), and is 1.4 °C (2.5 °F) warmer than during ...