Modelling the sea ice-ocean seasonal cycle in Hudson Bay, Foxe Basin and Hudson Strait, Canada |
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| Authors: | F J Saucier S Senneville S Prinsenberg F Roy G Smith P Gachon D Caya R Laprise |
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| Institution: | (1) Ocean Sciences Branch, Maurice Lamontagne Institute, Fisheries and Oceans Canada, 850 Route de la Mer, Mont-Joli, Qc G5H 3Z4, Canada;(2) Ocean Sciences Branch, Bedford Institute of Oceanography, Fisheries and Oceans Canada, Dartmouth, Canada;(3) Department of Atmospheric and Oceanic Sciences, McGill University, Montreal, Canada;(4) Meteorological Service of Canada, Montreal, Canada;(5) Ouranos Consortium on Climate Change, Montreal, Canada;(6) Department of Earth and Atmospheric Sciences, Université du Québec á Montreal, Montreal, Canada |
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| Abstract: | The seasonal cycle of water masses and sea ice in the Hudson Bay marine system is examined using a three-dimensional coastal ice-ocean model, with 10 km horizontal resolution and realistic tidal, atmospheric, hydrologic and oceanic forcing. The model includes a level 2.5 turbulent kinetic energy equation, multi-category elastic-viscous-plastic sea-ice rheology, and two layer sea ice with a single snow layer. Results from a two-year long model simulation between August 1996 and July 1998 are analyzed and compared with various observations. The results demonstrate a consistent seasonal cycle in atmosphere-ocean exchanges and the formation and circulation of water masses and sea ice. The model reproduces the summer and winter surface mixed layers, the general cyclonic circulation including the strong coastal current in eastern Hudson Bay, and the inflow of oceanic waters into Hudson Bay. The maximum sea-ice growth rates are found in western Foxe Basin, and in a relatively large and persistent polynya in northwestern Hudson Bay. Sea-ice advection and ridging are more important than local thermodynamic growth in the regions of maximum sea-ice cover concentration and thickness that are found in eastern Foxe Basin and southern Hudson Bay. The estimate of freshwater transport to the Labrador Sea confirms a broad maximum during wintertime that is associated with the previous summer s freshwater moving through Hudson Strait from southern Hudson Bay. Tidally driven mixing is shown to have a strong effect on the modeled ice-ocean circulation. |
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