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Dynamics of the Gulf of Maine
Joe Caracappa
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Geography and Topography
Bay of Fundy Georges Bank Scotian Shelf Northeast Channel Great South Channel Gulf of Maine Census, 2014
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Mean Currents Gulf of Maine Census, 2014 Bigelow, 1927
Maine Gyre – Counterclockwise Georges bank Gyre – Clockwise
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Water Masses Maine Surface Water (MSW) – Seasonally Variable
Maine Intermediate Water (MIW) – Coldest region, sourced by Scotian Current Maine Bottom Water (MBW) – High salinity, Gulf Stream origin Water Masses MSW MIW MBW Brooks, 1985
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Seasonal Changes Winter – Less Stratified, Slower mean currents
Summer – More Stratified, Faster gyration Satellite Oceanography Data Lab, University of Maine.& Naime et al, 1994.
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Biological Relevance JULY
Very Productive Fishery (Specifically Georges Bank) Peak landings ~35 million pounds (1990) Current landings ~ 4 million pounds Support Large coastal population in US and Canada OCTOBER APRIL
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References Bigelow, H. B Physical Oceanography of the Gulf of Maine. Fish Bull. 40: Brooks, David Vernal Circulation in the Gulf of Maine. Journal of Geophysical Research. 90: Greenberg, David Modeling the Mean Barotropic Circulation in the Bay of Fundy and Gulf of Maine. Journal of Physical Oceanography. 13: Lynch, Daniel et al Comprehensive coastal circulation model with application to the Gulf of Maine. Continental Shelf Research. 16: Naimie, Christopher et al Seasonal variation of the three- dimensional residual circulation on Georges Bank. Journal of Geophysical Research. 99:15,967-15,989. Satellite Oceanography Lab, University of Maine Gulf of Maine Census Bell,Tom Scientists, fishermen at odds on cod stock in Gulf of Maine. Portland Press Herald.
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