One general feature along the New England coast and continental shelf is that cold water on the Scotian Shelf (SS) moves southwestward, passing the Gulf of Maine (GoME) region before making its way to the downstream Mid-Atlantic Bight (Bisagni et al., 1996;Townsend et al., 2015). The GoME is a broad shallow sea along the US northeast coast extending from Cape Cod, US to Cape Sable, Canada. It is an important fishing ground due to its high biological productivity, especially around Georges Bank where the annual primary production can exceed 400 g[C]•m −2 yr −1 (Incze et al., 2010;Moriarty et al., 2016;Reilly et al., 1987). As an important driver for the GoME, the spatiotemporal variability of the upstream SS water is the focus of this study. Aspects of SS water impacts on GoME hydrodynamics will be further explored in a companion article (Li et al., 2021).The GoME is a strong tidally impacted region dominated by the semidiurnal M2 constituent (Greenberg, 1979;Xue et al., 2000). It is characterized by heterogeneous bathymetry and three separate deep basins (Georges, Jordan, and Wilkinson) that have depths larger than 200 m (Townsend et al., 2006). The GoME is semi-enclosed, and its exchange with the open Atlantic Ocean is largely restricted by Georges Bank and Browns Bank (BB). Slope water inflow to the GoME is through the narrow Northeast Channel between these two banks (Ramp et al., 1985), while the shallower Great South Channel located to the west of Georges Bank is a major exit of waters in the