Gulf Stream Sea Surface Temperature Anomalies Associated With the Extratropical Transition of North Atlantic Tropical Cyclones

Abstract This study investigates Gulf Stream (GS) sea surface temperature (SST) anomalies associated with the extratropical transition (ET) of tropical cyclones (TCs) in the North Atlantic. Composites of western North Atlantic TCs indicate that GS SSTs are warmer, and both large‐ and fine‐scale SST...

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Published in:Geophysical Research Letters
Main Authors: Evan Jones, Rhys Parfitt, Allison A. Wing, Robert Hart
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2023GL102904
https://doaj.org/article/ec0fa163563945928636efc805e9f06b
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spelling ftdoajarticles:oai:doaj.org/article:ec0fa163563945928636efc805e9f06b 2024-09-15T18:21:26+00:00 Gulf Stream Sea Surface Temperature Anomalies Associated With the Extratropical Transition of North Atlantic Tropical Cyclones Evan Jones Rhys Parfitt Allison A. Wing Robert Hart 2023-08-01T00:00:00Z https://doi.org/10.1029/2023GL102904 https://doaj.org/article/ec0fa163563945928636efc805e9f06b EN eng Wiley https://doi.org/10.1029/2023GL102904 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL102904 https://doaj.org/article/ec0fa163563945928636efc805e9f06b Geophysical Research Letters, Vol 50, Iss 16, Pp n/a-n/a (2023) extratropical transition western boundary current sea surface temperatures tropical cyclones frontogenesis Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2023GL102904 2024-08-05T17:49:23Z Abstract This study investigates Gulf Stream (GS) sea surface temperature (SST) anomalies associated with the extratropical transition (ET) of tropical cyclones (TCs) in the North Atlantic. Composites of western North Atlantic TCs indicate that GS SSTs are warmer, and both large‐ and fine‐scale SST gradients are weaker than average, for TCs that begin the ET process but do not complete it, compared with TCs that do. Further analysis suggests that the associated fine‐scale GS SST gradient anomalies are related to atmospheric processes but not the same as those that are typically associated with the onset of ET. As sensible heat flux gradients and surface diabatic frontogenesis are shown to generally scale with the local SST gradient strength, these results suggest that knowledge of the fine‐scale GS SST gradient in the weeks prior to the arrival of a TC might potentially provide additional information regarding the likelihood of that system completing ET. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 16
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic extratropical transition
western boundary current
sea surface temperatures
tropical cyclones
frontogenesis
Geophysics. Cosmic physics
QC801-809
spellingShingle extratropical transition
western boundary current
sea surface temperatures
tropical cyclones
frontogenesis
Geophysics. Cosmic physics
QC801-809
Evan Jones
Rhys Parfitt
Allison A. Wing
Robert Hart
Gulf Stream Sea Surface Temperature Anomalies Associated With the Extratropical Transition of North Atlantic Tropical Cyclones
topic_facet extratropical transition
western boundary current
sea surface temperatures
tropical cyclones
frontogenesis
Geophysics. Cosmic physics
QC801-809
description Abstract This study investigates Gulf Stream (GS) sea surface temperature (SST) anomalies associated with the extratropical transition (ET) of tropical cyclones (TCs) in the North Atlantic. Composites of western North Atlantic TCs indicate that GS SSTs are warmer, and both large‐ and fine‐scale SST gradients are weaker than average, for TCs that begin the ET process but do not complete it, compared with TCs that do. Further analysis suggests that the associated fine‐scale GS SST gradient anomalies are related to atmospheric processes but not the same as those that are typically associated with the onset of ET. As sensible heat flux gradients and surface diabatic frontogenesis are shown to generally scale with the local SST gradient strength, these results suggest that knowledge of the fine‐scale GS SST gradient in the weeks prior to the arrival of a TC might potentially provide additional information regarding the likelihood of that system completing ET.
format Article in Journal/Newspaper
author Evan Jones
Rhys Parfitt
Allison A. Wing
Robert Hart
author_facet Evan Jones
Rhys Parfitt
Allison A. Wing
Robert Hart
author_sort Evan Jones
title Gulf Stream Sea Surface Temperature Anomalies Associated With the Extratropical Transition of North Atlantic Tropical Cyclones
title_short Gulf Stream Sea Surface Temperature Anomalies Associated With the Extratropical Transition of North Atlantic Tropical Cyclones
title_full Gulf Stream Sea Surface Temperature Anomalies Associated With the Extratropical Transition of North Atlantic Tropical Cyclones
title_fullStr Gulf Stream Sea Surface Temperature Anomalies Associated With the Extratropical Transition of North Atlantic Tropical Cyclones
title_full_unstemmed Gulf Stream Sea Surface Temperature Anomalies Associated With the Extratropical Transition of North Atlantic Tropical Cyclones
title_sort gulf stream sea surface temperature anomalies associated with the extratropical transition of north atlantic tropical cyclones
publisher Wiley
publishDate 2023
url https://doi.org/10.1029/2023GL102904
https://doaj.org/article/ec0fa163563945928636efc805e9f06b
genre North Atlantic
genre_facet North Atlantic
op_source Geophysical Research Letters, Vol 50, Iss 16, Pp n/a-n/a (2023)
op_relation https://doi.org/10.1029/2023GL102904
https://doaj.org/toc/0094-8276
https://doaj.org/toc/1944-8007
1944-8007
0094-8276
doi:10.1029/2023GL102904
https://doaj.org/article/ec0fa163563945928636efc805e9f06b
op_doi https://doi.org/10.1029/2023GL102904
container_title Geophysical Research Letters
container_volume 50
container_issue 16
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