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Data collected during the Canadian Atlantic Storms Program (CASP) show subtidal variations in subsurface pressure (SSP) to be highly coherent throughout the Scotian Shelf region, and well correlated to fluctuations in the alongshelf component of wind stress (τy). Analysis using a frequency‐dependent multiple regression model verified that τy is the primary source of local forcing to the SSP field, although non‐locally generated variations in SSP are also important. The two components of local wind stress and a non‐local SSP term combine to explain over 90% of SSP variance on the Scotian Shelf. Statistical results describing the response to τy change dramatically depending upon the inclusion of non‐local forcing. In a model including both types of forcing, the SSP response to local forcing behaves like the solution to a dynamical model forced by time‐dependent wind stress with sea‐level prescribed to zero at the eastern cross‐shelf boundary. Local τy forcing becomes more effective to the west and ...

Subtidal response of the Scotian shelf bottom pressure field to meteorological forcing