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dc.contributor.authorChen, Changsheng  Concept link
dc.contributor.authorBeardsley, Robert C.  Concept link
dc.contributor.authorFranks, Peter J. S.  Concept link
dc.contributor.authorVan Keuren, J.  Concept link
dc.date.accessioned2010-05-25T14:17:32Z
dc.date.available2010-05-25T14:17:32Z
dc.date.issued2003-11-22
dc.identifier.citationJournal of Geophysical Research 108, C11 (2003): 8008en_US
dc.identifier.urihttps://hdl.handle.net/1912/3509
dc.descriptionAuthor Posting. © American Geophysical Union, 2003. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 108, C11 (2003): 8008, doi:10.1029/2001JC001245.en_US
dc.description.abstractThe influence of the diurnal heat flux on summer stratification and residual circulation over Georges Bank was examined using a three-dimensional primitive equation numerical circulation model. For a given spatially uniform and time-varying heat flux the model results show that the surface water is heated much faster on the southern flank than on the northern flank and much faster in the stratified region than in the mixed region. Heating significantly strengthens the tidal mixing front and intensifies the frontward convergence near the surface. As seasonal stratification develops, the location of the tidal mixing front gradually shifts on bank on the southern flank, while remaining almost unchanged on the northern flank. Response of the tidal currents to the diurnal variation in the heat flux varies across Georges Bank. It changes periodically with tidal cycles on the southern flank but is locked to the phase of the eastward tidal current on the northern flank. This phase-lock feature directly contributes to the intensification of the along-bank residual current jet on the northern flank. Diagnostic analysis suggests that this intensification is mainly caused by the heat-enhanced, cross-bank momentum flux. Model-computed variations of near-surface temperature and residual currents are in good agreement with satellite-derived sea surface temperature data and drifter measurements.en_US
dc.description.sponsorshipThis research was supported by the U.S. GLOBEC Northwest Atlantic/Georges Bank program through NOAA grants NA56RG0487, NA960P003, and NA960P005 to C. Chen, NSF grants OCE 96-32357, OCE 98-06379, and OCE 02-27679 to R. Beardsley, and NOAA grant NA76GP0176 to Peter Franks.en_US
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen_US
dc.publisherAmerican Geophysical Unionen_US
dc.relation.urihttps://doi.org/10.1029/2001JC001245
dc.subjectHeat fluxen_US
dc.subjectTidal mixing fronten_US
dc.subjectResidual currenten_US
dc.subjectStratificationen_US
dc.subjectFrontward convergenceen_US
dc.titleInfluence of diurnal heating on stratification and residual circulation of Georges Banken_US
dc.typeArticleen_US


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