Two regimes of the Arctic's circulation from ocean models with ice and contaminants.
A two-dimensional barotropic, coupled, ocean-ice model with a space resolution of 55.5 km and driven by atmospheric forces, river run-off, and sea-level slope between the Pacific and the Arctic Oceans, has been used to simulate the vertically averaged currents and ice drift in the Arctic Ocean. Results from 43 years of numerical simulations of water and ice motions demonstrate that two wind-driven circulation regimes are possible in the Arctic, a cyclonic and an anti-cyclonic circulation. These two regimes appear to alternate at 5-7 year intervals with the 10-15 year period. It is important to pollution studies to understand which circulation regime prevails at any time. It is anticipated that 1995 is a year with a cyclonic regime, and during this cyclonic phase and possibly during past cyclonic regimes as well, pollutants may reach the Alaskan shelf. The regime shifts demonstrated in this paper are fundamentally important to understanding the Arctic's general circulation and particularly important for estimating pollution transport.
Proshutinsky
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Institute of Marine Science, University of Alaska, Fairbanks 99775-7220, USA. aproshutinsky@whoi.edu
Johnson
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D001110:Arctic Regions; D004784:Environmental Monitoring; D007053:Ice; D008962:Models, Theoretical; D009792:Oceans and Seas; D012623:Seawater / Q000737:chemistry*; D014872:Water Movements; D014873:Water Pollutants / Q000032:analysis*; D014876:Water Pollution / Q000032:analysis*; D014919:Wind
D007053:Ice; D014873:Water Pollutants