COI Funded Project: Wintertime Watermass Evolution on the Outer Cape Cod Shelf
Project Funded: 2005
Key Words: Oceanography, Physical
Onset of wintertime cooling brings dramatic changes to the structure of coastal and shelf waters. The mixed layer deepens, penetrating to the bottom in shallow regions. As a result, a complex structure of mixing fronts evolves. This dynamic nearshore structure, in turn, has a profound effect on coastal circulation and distribution of biological and biogeochemical resources on the continental shelf. The depth of the mixed layer penetration and configuration of an emerging mixing front is determined by a number of interconnected factors: background temperature and salinity distribution, surface heat and freshwater fluxes, tidal and wind mixing. We propose a detailed study of wintertime changes in stratification of coastal waters east of Cape Cod, MA, relationship of these changes to atmospheric forcing, and their effect on the coastal and offshore ecosystems. The study will involve intensive Autonomous Underwater Vehicle sampling, combined with hydrographic, remote, and moored observations.
Originally published: January 1, 2005