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Volume 32 Issue 3
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Article Navigation >  Acta Oceanologica Sinica  > 2013  >  32(3): 54-62
XU Henglong, ZHU Mingzhuang, JIANG Yong, AL-RASHEID Khaled A S. Temporal species distributions of planktonic protist communities in semi-enclosed mariculture waters and responses to environmental stress[J]. Acta Oceanologica Sinica, 2010, (3): 74-83. doi: 10.1007/s13131-010-0038-7
Citation: LI Qun, ZHANG Zhanhai, WU Huiding. Interaction of an anticyclonic eddy with sea ice in the western Arctic Ocean: an eddy-resolving model study[J]. Acta Oceanologica Sinica, 2013, 32(3): 54-62. doi: 10.1007/s13131-013-0289-1
shu

Interaction of an anticyclonic eddy with sea ice in the western Arctic Ocean: an eddy-resolving model study

doi: 10.1007/s13131-013-0289-1
  • 1.

    Polar Research Institute of China, State Oceanic Administration, Shanghai 200136, China

  • 2.

    Polar Research Institute of China, State Oceanic Administration, Shanghai 200136, China;National Marine Environmental Forecasting Center, State Oceanic Administration, Beijing 100081, China

  • Received Date: 2011-10-08
  • Rev Recd Date: 2012-05-03
    Abstract
  • The dramatic decline of summer sea ice extent and thickness has been witnessed in the western Arctic Ocean in recent decades, which has motivated scientists to search for possible factors driving the sea ice variability. An eddy-resolving, ice-ocean coupled model covering the entire Arctic Ocean is implemented, with focus on the western Arctic Ocean. Special attention is paid to the summer Alaskan coastal current (ACC), which has a high temperature (up to 5℃ or more) in the upper layer due to the solar radiation over the open water at the lower latitude. Downstream of the ACC after Barrow Point, a surface-intensified anticyclonic eddy is frequently generated and propagate towards the Canada Basin during the summer season when sea ice has retreated away from the coast. Such an eddy has a warm core, and its source is high-temperature ACC water. A typical warm-core eddy is traced. It is trapped just below summer sea ice melt water and has a thickness about 60 m. Temperature in the eddy core reaches 2-3℃, and most water inside the eddy has a temperature over 1℃. With a definition of the eddy boundary, an eddy heat is calculated, which can melt 1 600 km2 of 1 m thick sea ice under extreme conditions.
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