The effect of lower sea level on geostrophic transport through the Florida Straits during the last glacial maximum

We investigate the effect of a 120 meter sea level drop on transport through the Caribbean Sea and the Florida Straits during the Last Glacial Maximum (LGM) relative to the present, using the Regional Ocean Modeling System (ROMS). A geostrophic transport estimate for the Florida Straits suggests the...

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Bibliographic Details
Main Author: Ionita, Dana
Other Authors: Lynch-Stieglitz, Jean, Di Lorenzo, Emanuele, Earth and Atmospheric Sciences, Annalisa Bracco, Robert Black
Format: Thesis
Language:unknown
Published: Georgia Institute of Technology 2009
Subjects:
LGM
Online Access:http://hdl.handle.net/1853/28200
id ftgeorgiatech:oai:smartech.gatech.edu:1853/28200
record_format openpolar
spelling ftgeorgiatech:oai:smartech.gatech.edu:1853/28200 2023-05-15T17:33:31+02:00 The effect of lower sea level on geostrophic transport through the Florida Straits during the last glacial maximum Ionita, Dana Lynch-Stieglitz, Jean Di Lorenzo, Emanuele Earth and Atmospheric Sciences Annalisa Bracco Robert Black 2009-01-14 application/pdf http://hdl.handle.net/1853/28200 unknown Georgia Institute of Technology http://hdl.handle.net/1853/28200 Geostrophic transport Florida Straits LGM Last Glacial Maximum Sea level Geostrophic currents Florida Straits of Text Thesis 2009 ftgeorgiatech 2023-02-13T18:45:48Z We investigate the effect of a 120 meter sea level drop on transport through the Caribbean Sea and the Florida Straits during the Last Glacial Maximum (LGM) relative to the present, using the Regional Ocean Modeling System (ROMS). A geostrophic transport estimate for the Florida Straits suggests the LGM Florida Current was weaker than today by one third, inferring a likely decrease in the North Atlantic overturning circulation by 12-15 Sv. A possible impact of a shallower LGM Florida Straits sill depth on the Florida Current has been suggested. Our model results show that the volume transport through the Florida Straits is slightly reduced in a lower sea level model simulation when compared to a control sea level simulation (34.8 ± 2.0 Sv vs. 39.8 ± 2.3 Sv). The difference in transport is of the order of 5 Sv, representing a maximum limit to the LGM flow reduction due to sea level change. Therefore the change in sill depth between the LGM and the present is unlikely to have been a cause of the entire observed flow reduction. M.S. Thesis North Atlantic Georgia Institute of Technology: SMARTech - Scholarly Materials and Research at Georgia Tech
institution Open Polar
collection Georgia Institute of Technology: SMARTech - Scholarly Materials and Research at Georgia Tech
op_collection_id ftgeorgiatech
language unknown
topic Geostrophic transport
Florida Straits
LGM
Last Glacial Maximum
Sea level
Geostrophic currents
Florida
Straits of
spellingShingle Geostrophic transport
Florida Straits
LGM
Last Glacial Maximum
Sea level
Geostrophic currents
Florida
Straits of
Ionita, Dana
The effect of lower sea level on geostrophic transport through the Florida Straits during the last glacial maximum
topic_facet Geostrophic transport
Florida Straits
LGM
Last Glacial Maximum
Sea level
Geostrophic currents
Florida
Straits of
description We investigate the effect of a 120 meter sea level drop on transport through the Caribbean Sea and the Florida Straits during the Last Glacial Maximum (LGM) relative to the present, using the Regional Ocean Modeling System (ROMS). A geostrophic transport estimate for the Florida Straits suggests the LGM Florida Current was weaker than today by one third, inferring a likely decrease in the North Atlantic overturning circulation by 12-15 Sv. A possible impact of a shallower LGM Florida Straits sill depth on the Florida Current has been suggested. Our model results show that the volume transport through the Florida Straits is slightly reduced in a lower sea level model simulation when compared to a control sea level simulation (34.8 ± 2.0 Sv vs. 39.8 ± 2.3 Sv). The difference in transport is of the order of 5 Sv, representing a maximum limit to the LGM flow reduction due to sea level change. Therefore the change in sill depth between the LGM and the present is unlikely to have been a cause of the entire observed flow reduction. M.S.
author2 Lynch-Stieglitz, Jean
Di Lorenzo, Emanuele
Earth and Atmospheric Sciences
Annalisa Bracco
Robert Black
format Thesis
author Ionita, Dana
author_facet Ionita, Dana
author_sort Ionita, Dana
title The effect of lower sea level on geostrophic transport through the Florida Straits during the last glacial maximum
title_short The effect of lower sea level on geostrophic transport through the Florida Straits during the last glacial maximum
title_full The effect of lower sea level on geostrophic transport through the Florida Straits during the last glacial maximum
title_fullStr The effect of lower sea level on geostrophic transport through the Florida Straits during the last glacial maximum
title_full_unstemmed The effect of lower sea level on geostrophic transport through the Florida Straits during the last glacial maximum
title_sort effect of lower sea level on geostrophic transport through the florida straits during the last glacial maximum
publisher Georgia Institute of Technology
publishDate 2009
url http://hdl.handle.net/1853/28200
genre North Atlantic
genre_facet North Atlantic
op_relation http://hdl.handle.net/1853/28200
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