Accelerated sea level rise and Florida Current transport
The Florida Current is the headwater of the Gulf Stream and is a component of the North Atlantic western boundary current from which a geostrophic balance between sea surface height and mass transport directly influence coastal sea levels along the Florida Straits. A linear regression of daily Flori...
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Copernicus Publications
2015
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fttriple:oai:gotriple.eu:oai:doaj.org/article:5b12ba56e73a4590a9f4ee1759573b91 2023-05-15T17:32:49+02:00 Accelerated sea level rise and Florida Current transport J. Park W. Sweet 2015-07-01 https://doi.org/10.5194/os-11-607-2015 http://www.ocean-sci.net/11/607/2015/os-11-607-2015.pdf https://doaj.org/article/5b12ba56e73a4590a9f4ee1759573b91 en eng Copernicus Publications 1812-0784 1812-0792 doi:10.5194/os-11-607-2015 http://www.ocean-sci.net/11/607/2015/os-11-607-2015.pdf https://doaj.org/article/5b12ba56e73a4590a9f4ee1759573b91 undefined Ocean Science, Vol 11, Iss 4, Pp 607-615 (2015) envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2015 fttriple https://doi.org/10.5194/os-11-607-2015 2023-01-22T19:11:20Z The Florida Current is the headwater of the Gulf Stream and is a component of the North Atlantic western boundary current from which a geostrophic balance between sea surface height and mass transport directly influence coastal sea levels along the Florida Straits. A linear regression of daily Florida Current transport estimates does not find a significant change in transport over the last decade; however, a nonlinear trend extracted from empirical mode decomposition (EMD) suggests a 3 Sv decline in mean transport. This decline is consistent with observed tide gauge records in Florida Bay and the straits exhibiting an acceleration of mean sea level (MSL) rise over the decade. It is not known whether this recent change represents natural variability or the onset of the anticipated secular decline in Atlantic meridional overturning circulation (AMOC); nonetheless, such changes have direct impacts on the sensitive ecological systems of the Everglades as well as the climate of western Europe and eastern North America. Article in Journal/Newspaper North Atlantic Unknown Ocean Science 11 4 607 615 |
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envir geo J. Park W. Sweet Accelerated sea level rise and Florida Current transport |
topic_facet |
envir geo |
description |
The Florida Current is the headwater of the Gulf Stream and is a component of the North Atlantic western boundary current from which a geostrophic balance between sea surface height and mass transport directly influence coastal sea levels along the Florida Straits. A linear regression of daily Florida Current transport estimates does not find a significant change in transport over the last decade; however, a nonlinear trend extracted from empirical mode decomposition (EMD) suggests a 3 Sv decline in mean transport. This decline is consistent with observed tide gauge records in Florida Bay and the straits exhibiting an acceleration of mean sea level (MSL) rise over the decade. It is not known whether this recent change represents natural variability or the onset of the anticipated secular decline in Atlantic meridional overturning circulation (AMOC); nonetheless, such changes have direct impacts on the sensitive ecological systems of the Everglades as well as the climate of western Europe and eastern North America. |
format |
Article in Journal/Newspaper |
author |
J. Park W. Sweet |
author_facet |
J. Park W. Sweet |
author_sort |
J. Park |
title |
Accelerated sea level rise and Florida Current transport |
title_short |
Accelerated sea level rise and Florida Current transport |
title_full |
Accelerated sea level rise and Florida Current transport |
title_fullStr |
Accelerated sea level rise and Florida Current transport |
title_full_unstemmed |
Accelerated sea level rise and Florida Current transport |
title_sort |
accelerated sea level rise and florida current transport |
publisher |
Copernicus Publications |
publishDate |
2015 |
url |
https://doi.org/10.5194/os-11-607-2015 http://www.ocean-sci.net/11/607/2015/os-11-607-2015.pdf https://doaj.org/article/5b12ba56e73a4590a9f4ee1759573b91 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Ocean Science, Vol 11, Iss 4, Pp 607-615 (2015) |
op_relation |
1812-0784 1812-0792 doi:10.5194/os-11-607-2015 http://www.ocean-sci.net/11/607/2015/os-11-607-2015.pdf https://doaj.org/article/5b12ba56e73a4590a9f4ee1759573b91 |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/os-11-607-2015 |
container_title |
Ocean Science |
container_volume |
11 |
container_issue |
4 |
container_start_page |
607 |
op_container_end_page |
615 |
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1766131093701918720 |