“…The interior GOM is comprised of three basins with depths greater than 200m -Georges Basin, Wilkinson Basin, and Jordan Basin -and is separated from the open North Atlantic via offshore banks shallower than 100m -Georges Bank and Browns Bank. The general circulation in the GOM is cyclonic, with anticyclonic circulation around Georges Bank (Bigelow, 1927;Brooks, 1994;Xue et al, 2000). Alongshore flow on the coast of Maine is divided into the buoyancy-driven Maine Coastal Current, and the GOM Coastal Plume (Bisagni et al, 1996;Keafer et al, 2005;Pettigrew et al, 2005), which is fed by the region's five largest rivers, the St. John, Penobscot, Merrimack, Kennebec, and…”