Observations of the vertical and temporal evolution of a Natal Pulse along the Eastern Agulhas Bank
This study re-investigates the work of Lutjeharms et al. [2001,2003] who documented the properties of a Natal Pulse using isopycnal Lagrangian floats. We combined Lagrangian analyses and Eulerian maps derived from objective analysis to better describe the evolution of a Natal Pulse along three densi...
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ftarchimer:oai:archimer.ifremer.fr:46162 2023-05-15T13:50:50+02:00 Observations of the vertical and temporal evolution of a Natal Pulse along the Eastern Agulhas Bank Pivan, Xavier Krug, Marjolaine Herbette, Steven 2016-09 application/pdf https://archimer.ifremer.fr/doc/00350/46162/45860.pdf https://doi.org/10.1002/2015JC011582 https://archimer.ifremer.fr/doc/00350/46162/ eng eng Amer Geophysical Union https://archimer.ifremer.fr/doc/00350/46162/45860.pdf doi:10.1002/2015JC011582 https://archimer.ifremer.fr/doc/00350/46162/ 2016. American Geophysical Union. All Rights Reserved. info:eu-repo/semantics/openAccess restricted use Journal Of Geophysical Research-oceans (2169-9275) (Amer Geophysical Union), 2016-09 , Vol. 121 , N. 9 , P. 7108-7122 Agulhas Current Natal Pulse Lagrangian floats text Publication info:eu-repo/semantics/article 2016 ftarchimer https://doi.org/10.1002/2015JC011582 2021-09-23T20:28:47Z This study re-investigates the work of Lutjeharms et al. [2001,2003] who documented the properties of a Natal Pulse using isopycnal Lagrangian floats. We combined Lagrangian analyses and Eulerian maps derived from objective analysis to better describe the evolution of a Natal Pulse along three density surfaces referred to as the surface (satellite-observed), shallow (isopycnal-1026.8 kg.m−3) and deep (isopycnal-1027.2 kg.m−3) layer. Our observations show that this Natal Pulse extended to a depth of 1000m and was associated with cyclonic relative vorticity values of about 6.5 to 8.5x10−5.s−1 in the surface and shallow layer and 4x10−5.s−1 in the deep layer. This Natal Pulse contributed to cross-shelf exchange through the offshore advection of Eastern Agulhas Bank water near the surface, onshore advection of South Indian Central Water and/or Indian Equatorial Water in the shallow layer and Antarctic Intermediate Water in the deep layer. Sea Surface Temperature maps showed that the downstream progression of the Natal Pulse along the 3000m isobath was related to a readjustment of its rotation axis. This readjustment advected Eastern Agulhas Bank water into the Natal Pulse eddy and triggered a SST cooling of about 3°C in the cyclonic area. The importance of a warm recirculating Agulhas plume originating from the Natal Pulse was highlighted. This warm water plume extended to a depth of 700m and was associated with onshore velocities exceeding those experienced within the Natal Pulse eddy by a factor of two. Our observations indicate that the June/July 1998 Natal Pulse and its associated plumes enhanced cross-shelf exchanges. This article is protected by copyright. All rights reserved. Article in Journal/Newspaper Antarc* Antarctic Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Antarctic Indian Journal of Geophysical Research: Oceans 121 9 7108 7122 |
institution |
Open Polar |
collection |
Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) |
op_collection_id |
ftarchimer |
language |
English |
topic |
Agulhas Current Natal Pulse Lagrangian floats |
spellingShingle |
Agulhas Current Natal Pulse Lagrangian floats Pivan, Xavier Krug, Marjolaine Herbette, Steven Observations of the vertical and temporal evolution of a Natal Pulse along the Eastern Agulhas Bank |
topic_facet |
Agulhas Current Natal Pulse Lagrangian floats |
description |
This study re-investigates the work of Lutjeharms et al. [2001,2003] who documented the properties of a Natal Pulse using isopycnal Lagrangian floats. We combined Lagrangian analyses and Eulerian maps derived from objective analysis to better describe the evolution of a Natal Pulse along three density surfaces referred to as the surface (satellite-observed), shallow (isopycnal-1026.8 kg.m−3) and deep (isopycnal-1027.2 kg.m−3) layer. Our observations show that this Natal Pulse extended to a depth of 1000m and was associated with cyclonic relative vorticity values of about 6.5 to 8.5x10−5.s−1 in the surface and shallow layer and 4x10−5.s−1 in the deep layer. This Natal Pulse contributed to cross-shelf exchange through the offshore advection of Eastern Agulhas Bank water near the surface, onshore advection of South Indian Central Water and/or Indian Equatorial Water in the shallow layer and Antarctic Intermediate Water in the deep layer. Sea Surface Temperature maps showed that the downstream progression of the Natal Pulse along the 3000m isobath was related to a readjustment of its rotation axis. This readjustment advected Eastern Agulhas Bank water into the Natal Pulse eddy and triggered a SST cooling of about 3°C in the cyclonic area. The importance of a warm recirculating Agulhas plume originating from the Natal Pulse was highlighted. This warm water plume extended to a depth of 700m and was associated with onshore velocities exceeding those experienced within the Natal Pulse eddy by a factor of two. Our observations indicate that the June/July 1998 Natal Pulse and its associated plumes enhanced cross-shelf exchanges. This article is protected by copyright. All rights reserved. |
format |
Article in Journal/Newspaper |
author |
Pivan, Xavier Krug, Marjolaine Herbette, Steven |
author_facet |
Pivan, Xavier Krug, Marjolaine Herbette, Steven |
author_sort |
Pivan, Xavier |
title |
Observations of the vertical and temporal evolution of a Natal Pulse along the Eastern Agulhas Bank |
title_short |
Observations of the vertical and temporal evolution of a Natal Pulse along the Eastern Agulhas Bank |
title_full |
Observations of the vertical and temporal evolution of a Natal Pulse along the Eastern Agulhas Bank |
title_fullStr |
Observations of the vertical and temporal evolution of a Natal Pulse along the Eastern Agulhas Bank |
title_full_unstemmed |
Observations of the vertical and temporal evolution of a Natal Pulse along the Eastern Agulhas Bank |
title_sort |
observations of the vertical and temporal evolution of a natal pulse along the eastern agulhas bank |
publisher |
Amer Geophysical Union |
publishDate |
2016 |
url |
https://archimer.ifremer.fr/doc/00350/46162/45860.pdf https://doi.org/10.1002/2015JC011582 https://archimer.ifremer.fr/doc/00350/46162/ |
geographic |
Antarctic Indian |
geographic_facet |
Antarctic Indian |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
Journal Of Geophysical Research-oceans (2169-9275) (Amer Geophysical Union), 2016-09 , Vol. 121 , N. 9 , P. 7108-7122 |
op_relation |
https://archimer.ifremer.fr/doc/00350/46162/45860.pdf doi:10.1002/2015JC011582 https://archimer.ifremer.fr/doc/00350/46162/ |
op_rights |
2016. American Geophysical Union. All Rights Reserved. info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.1002/2015JC011582 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
121 |
container_issue |
9 |
container_start_page |
7108 |
op_container_end_page |
7122 |
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1766254156365955072 |