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Everything about Bering Sea totally explained

The Bering (or Imarpik) Sea is a body of water in the Pacific Ocean that comprises a deep water basin (the Aleutian Basin) which rises through a narrow slope into the shallower water above the continental shelves.
   The Bering Sea is separated from the Gulf of Alaska by the Alaska Peninsula and Aleutian Islands. Covering over two million square kilometers (775,000 sq mi), it's bordered on the east and northeast by Alaska, on the west by Russia's Siberia and Kamchatka Peninsula, on the south by the Alaska Peninsula and the Aleutian Islands and on the far north by the Bering Strait which separates the Bering Sea from the Arctic Ocean's Chukchi Sea. Bristol Bay is the portion of the Bering Sea which separates the Alaska Peninsula from mainland Alaska. The Bering Sea is named for the first European discoverer to sail its waters, the Danish navigator Vitus Bering.
   The Bering Sea ecosystem includes resources within the jurisdiction of the United States and Russia, as well as international waters in the ‘Donut Hole’. The interaction between currents, sea ice, and weather make for a vigorous and productive ecosystem.

History

Most scientists believe that during the most recent ice age, sea level was low enough to allow humans and other animals to migrate on foot from Asia to North America across what is now the Bering Strait. This is commonly referred to as the "Bering land bridge" and is believed by some—though not all—scholars to be the first point of entry of humans into the Americas.
   There is a small portion of the Kula Plate in the Bering Sea. The Kula Plate is an ancient tectonic plate that used to subduct under Alaska during the Triassic period.

Geography

Islands of the Bering Sea include:
Regions of the Bering Sea include
  • Bering Strait
  • Bristol Bay The Bering Sea contains 16 submarine canyons including the largest submarine canyon in the world, Zhemchug canyon.

    Ecosystem

    The Bering Sea Shelf break is the dominant driver of primary productivity in the Bering Sea. This zone, where the shallower continental shelf drops off into the Aleutian Basin is also known as the “Greenbelt”. Nutrient upwelling from the cold waters of the Aleutian basin flowing up the slope and mixing with shallower waters of the shelf provide for constant production of phytoplankton.
       The second driver of productivity in the Bering Sea is seasonal sea ice that, in part, triggers the spring phytoplankton bloom. Seasonal melting of sea ice causes an influx of lower salinity water into the middle and other shelf areas, causing stratification and hydrographic effects which influence productivity. In addition to the hydrographic and productivity influence of melting sea ice, the ice itself also provides an attachment substrate for the growth of algae as well as interstitial ice algae. The productivity associated with sea ice is under threat as global warming causes a reduction of sea ice in the Bering Sea.
       Some evidence suggests that great changes to the Bering Sea ecosystem have already occurred. Warm water conditions in the summer of 1997 resulted in a massive bloom of low energy coccolithophorid phytoplankton (Stockwell et al. 2001). A long record of carbon isotopes, which is reflective of primary production trends of the Bering Sea, exists from historical samples of bowhead whale baleen. Trends in carbon isotope ratios in whale baleen samples suggest that a 30-40% decline in average seasonal primary productivity has occurred over the last 50 years. opilio and tanner crabs, Bristol Bay salmon, pollock and other groundfish. These fisheries rely on the productivity of the Bering Sea via a complicated and little understood food web. The continued existence of these fisheries requires an intact, healthy, and productive ecosystem.
       Commercial fishing is big business in the Bering Sea. Some of the largest seafood companies in the world rely on the Bering Sea to produce fish and shellfish. On the U.S. side, commercial fisheries in the Bering Sea catch approximately $1 billion worth of seafood annually, while Russian Bering Sea fisheries are worth approximately $600 million annually. Hit TV Show Deadliest Catch shows the lives of crab Fishermen on the Bering Sea.

    Links to Bering Sea data

    The Bering Sea supports some of the world's richest fisheries, and landings from Alaskan waters represents half the U.S. catch of fish and shellfish. Because of the changes going on in the Arctic, future evolution of the Bering Sea climate/ecosystem is more uncertain. This is a symmetric problem: climate change impacts ecosystems, and ecosystems serve as indicators for climate change. Track the current State of the Bering Sea with near-realtime ecological and climatic indicators.

    Further Information

    Get more info on 'Bering Sea'.


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