Influence of diurnal heating on stratification and residual circulation of Georges Bank
Author 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. The influence...
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ftwhoas:oai:darchive.mblwhoilibrary.org:1912/3509 2023-05-15T17:45:46+02:00 Influence of diurnal heating on stratification and residual circulation of Georges Bank Chen, Changsheng Beardsley, Robert C. Franks, Peter J. S. Van Keuren, J. 2003-11-22 application/pdf https://hdl.handle.net/1912/3509 en_US eng American Geophysical Union https://doi.org/10.1029/2001JC001245 Journal of Geophysical Research 108, C11 (2003): 8008 https://hdl.handle.net/1912/3509 Journal of Geophysical Research 108, C11 (2003): 8008 Heat flux Tidal mixing front Residual current Stratification Frontward convergence Article 2003 ftwhoas https://doi.org/10.1029/2001JC001245 2022-05-28T22:58:00Z Author 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. The 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. This 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. Article in Journal/Newspaper Northwest Atlantic Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Journal of Geophysical Research 108 C11 |
institution |
Open Polar |
collection |
Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
op_collection_id |
ftwhoas |
language |
English |
topic |
Heat flux Tidal mixing front Residual current Stratification Frontward convergence |
spellingShingle |
Heat flux Tidal mixing front Residual current Stratification Frontward convergence Chen, Changsheng Beardsley, Robert C. Franks, Peter J. S. Van Keuren, J. Influence of diurnal heating on stratification and residual circulation of Georges Bank |
topic_facet |
Heat flux Tidal mixing front Residual current Stratification Frontward convergence |
description |
Author 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. The 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. This 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. |
format |
Article in Journal/Newspaper |
author |
Chen, Changsheng Beardsley, Robert C. Franks, Peter J. S. Van Keuren, J. |
author_facet |
Chen, Changsheng Beardsley, Robert C. Franks, Peter J. S. Van Keuren, J. |
author_sort |
Chen, Changsheng |
title |
Influence of diurnal heating on stratification and residual circulation of Georges Bank |
title_short |
Influence of diurnal heating on stratification and residual circulation of Georges Bank |
title_full |
Influence of diurnal heating on stratification and residual circulation of Georges Bank |
title_fullStr |
Influence of diurnal heating on stratification and residual circulation of Georges Bank |
title_full_unstemmed |
Influence of diurnal heating on stratification and residual circulation of Georges Bank |
title_sort |
influence of diurnal heating on stratification and residual circulation of georges bank |
publisher |
American Geophysical Union |
publishDate |
2003 |
url |
https://hdl.handle.net/1912/3509 |
genre |
Northwest Atlantic |
genre_facet |
Northwest Atlantic |
op_source |
Journal of Geophysical Research 108, C11 (2003): 8008 |
op_relation |
https://doi.org/10.1029/2001JC001245 Journal of Geophysical Research 108, C11 (2003): 8008 https://hdl.handle.net/1912/3509 |
op_doi |
https://doi.org/10.1029/2001JC001245 |
container_title |
Journal of Geophysical Research |
container_volume |
108 |
container_issue |
C11 |
_version_ |
1766149009806721024 |