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Low-frequency current variability on the southern mid-Atlantic bight

Journal Article · · J. Phys. Oceanogr.; (United States)
Low-frequency current variability on the continental shelf, 84 km off the mouth of the Chesapeake Bay, was examined from 4-month (mid-March to June 1975) current, sea level and meterological records. Taking into account the seasonal change in wind stress and stratification, the record was divided into two 60-day periods. In both periods, the transient alongshore currents were barotropic and coherent with sea level fluctuations.During the first period (March and April 1975), winds were in the east--west direction, and the shelf water was homogeneous. At time scales longer than 4 days, sea level was a large-scale feature (coherent over the entire Mid-Atlantic Bight). At shorter time scales, sea level was driven by the local, alongshore wind. In contrast, the cross-shelf current, which was mainly barotropic, was driven by the alongshore wind at all time scales.During the second period (May and June 1975), winds were in the north-south direction and the shelfwater was stratified. Sea level was mainly driven by the local alongshore wind at all time scales. The cross-shelf current, which was baroclinic at time scales longer than 4 days, and barotropic at shorter time scales, was also driven by the alongshore wind.The difference in response characteristics of the two periods indicate that circulation on the southern Mid-Atlantic Bight is strongly affected by local wind forcing, nonlocal effect, density stratification and the duration of alongshore wind.
Research Organization:
Department of Earth and Planetary Sciences, The Johns Hopkins University, Baltimore, MD 21218
OSTI ID:
5792629
Journal Information:
J. Phys. Oceanogr.; (United States), Journal Name: J. Phys. Oceanogr.; (United States) Vol. 9:6; ISSN JPYOB
Country of Publication:
United States
Language:
English

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