Ocean Observing and Modeling Group

 

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Frontal Interaction and Atmospheric Forcing North of Cape Hatteras, an Analysis and Modeling Study

 

 

Funding period: 2009-2012

 

Collaborators

WHOI – G. Gawarkiewicz, J. Churchill

 

Project Summary

 

Strong shelf flows are found in close proximity with large-scale deep ocean boundary currents in many areas of the world oceans.  The interaction of shelf flows with an open-ocean boundary current can be of tremendous importance as it often results in significant export of coastal water to the deep ocean.  However, the dynamics of this interaction are not well understood, and may not be well represented in regional or larger scale numerical models of ocean circulation.  We propose a comprehensive study of the interaction of the Gulf Stream with the shelf-edge frontal jet of the Middle Atlantic Bight.  This is likely the best know example of shelf/boundary current interaction, but has not been the explicit focus of a scientific study.  Our study will combine analysis of data from intensive field projects with idealized and real-ocean numerical modeling.  The modeling and data analysis will be closely coupled. The data analysis providing insight to the processes under consideration and be used to assess and refine the model’s performance.  The model will, in turn, be used to examine the dynamics of the current interaction in a much finer spatial and temporal detail than possible with actual measurements.  Our overall objectives will be to better understand:

·   The interaction of the shelfbreak front, and frontal jet, with the Gulf Stream and atmospheric forcing

·   How the outer and mid-shelf flow is influenced by atmospheric forcing and by incursions of the Gulf Stream onto the mid- and upper-slope offshore

·   How the shelf dynamics is influenced by the narrowing shelf width approaching Cape Hatteras (considering especially vorticity constraints and the changing role of Gulf Stream forcing on the shelf currents)

When completed, our project will not only have forwarded the understanding of the interaction of the Gulf Stream with the shelf break frontal jet, but have led to a greater understanding of similar current interactions that occur throughout the world’s oceans.

 

Results