Ekman Transport as the Driver of Extreme Interannual Formation Rates of Eighteen Degree Water
International audience The EDW is a nearly homogeneous water body found in the western subtropical North Atlantic region. That was named after the fact that it maintains a nearly constant temperature around 18°C. The EDW is primarily formed to the west of 45°W, between the Gulf Stream and 30°N (Maze...
Published in: | Journal of Geophysical Research: Oceans |
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Online Access: | https://hal.archives-ouvertes.fr/hal-03814771 https://hal.archives-ouvertes.fr/hal-03814771/document https://hal.archives-ouvertes.fr/hal-03814771/file/90674.pdf https://doi.org/10.1029/2021jc017696 |
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ftunivnantes:oai:HAL:hal-03814771v1 2023-05-15T17:33:51+02:00 Ekman Transport as the Driver of Extreme Interannual Formation Rates of Eighteen Degree Water Li, Ke Maze, Guillaume Mercier, Herlé Laboratoire d'Océanographie Physique et Spatiale (LOPS) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS) 2022 https://hal.archives-ouvertes.fr/hal-03814771 https://hal.archives-ouvertes.fr/hal-03814771/document https://hal.archives-ouvertes.fr/hal-03814771/file/90674.pdf https://doi.org/10.1029/2021jc017696 en eng HAL CCSD Wiley-Blackwell info:eu-repo/semantics/altIdentifier/doi/10.1029/2021jc017696 hal-03814771 https://hal.archives-ouvertes.fr/hal-03814771 https://hal.archives-ouvertes.fr/hal-03814771/document https://hal.archives-ouvertes.fr/hal-03814771/file/90674.pdf doi:10.1029/2021jc017696 info:eu-repo/semantics/OpenAccess ISSN: 2169-9275 EISSN: 2169-9291 Journal of Geophysical Research. Oceans https://hal.archives-ouvertes.fr/hal-03814771 Journal of Geophysical Research. Oceans, Wiley-Blackwell, 2022, 127 (1), pp.e2021JC017696. ⟨10.1029/2021jc017696⟩ [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography info:eu-repo/semantics/article Journal articles 2022 ftunivnantes https://doi.org/10.1029/2021jc017696 2022-10-18T23:01:59Z International audience The EDW is a nearly homogeneous water body found in the western subtropical North Atlantic region. That was named after the fact that it maintains a nearly constant temperature around 18°C. The EDW is primarily formed to the west of 45°W, between the Gulf Stream and 30°N (Maze et al., 2009). In this region, the air-sea heat flux in EDW is the key driving mechanism of EDW formation and destruction in the seasonal time scale (Forget et al., 2011; Maze et al., 2009). Maze et al. (2009) showed that in a typical seasonal cycle, intense winter surface buoyancy loss leads to the outcropping of EDW, which is replenished during this period. In the spring and summer, surface buoyancy flux destroys the EDW. Over the 2004-2006 period, Forget et al. (2011) examined the EDW volume and reported that the EDW volume increase peaked at 8.6 Svy (Sverdrup year, 1 Svy = 3.154 × 10 13 m 3) in February, with a total EDW volume increase due to air-sea heat fluxes of 9.3 Svy. The EDW destruction due to air-sea heat fluxes was −4.6 Svy, and that due to mixing was −2.6 Svy. The net annual Article in Journal/Newspaper North Atlantic Université de Nantes: HAL-UNIV-NANTES Journal of Geophysical Research: Oceans 127 1 |
institution |
Open Polar |
collection |
Université de Nantes: HAL-UNIV-NANTES |
op_collection_id |
ftunivnantes |
language |
English |
topic |
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography |
spellingShingle |
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography Li, Ke Maze, Guillaume Mercier, Herlé Ekman Transport as the Driver of Extreme Interannual Formation Rates of Eighteen Degree Water |
topic_facet |
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography |
description |
International audience The EDW is a nearly homogeneous water body found in the western subtropical North Atlantic region. That was named after the fact that it maintains a nearly constant temperature around 18°C. The EDW is primarily formed to the west of 45°W, between the Gulf Stream and 30°N (Maze et al., 2009). In this region, the air-sea heat flux in EDW is the key driving mechanism of EDW formation and destruction in the seasonal time scale (Forget et al., 2011; Maze et al., 2009). Maze et al. (2009) showed that in a typical seasonal cycle, intense winter surface buoyancy loss leads to the outcropping of EDW, which is replenished during this period. In the spring and summer, surface buoyancy flux destroys the EDW. Over the 2004-2006 period, Forget et al. (2011) examined the EDW volume and reported that the EDW volume increase peaked at 8.6 Svy (Sverdrup year, 1 Svy = 3.154 × 10 13 m 3) in February, with a total EDW volume increase due to air-sea heat fluxes of 9.3 Svy. The EDW destruction due to air-sea heat fluxes was −4.6 Svy, and that due to mixing was −2.6 Svy. The net annual |
author2 |
Laboratoire d'Océanographie Physique et Spatiale (LOPS) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Li, Ke Maze, Guillaume Mercier, Herlé |
author_facet |
Li, Ke Maze, Guillaume Mercier, Herlé |
author_sort |
Li, Ke |
title |
Ekman Transport as the Driver of Extreme Interannual Formation Rates of Eighteen Degree Water |
title_short |
Ekman Transport as the Driver of Extreme Interannual Formation Rates of Eighteen Degree Water |
title_full |
Ekman Transport as the Driver of Extreme Interannual Formation Rates of Eighteen Degree Water |
title_fullStr |
Ekman Transport as the Driver of Extreme Interannual Formation Rates of Eighteen Degree Water |
title_full_unstemmed |
Ekman Transport as the Driver of Extreme Interannual Formation Rates of Eighteen Degree Water |
title_sort |
ekman transport as the driver of extreme interannual formation rates of eighteen degree water |
publisher |
HAL CCSD |
publishDate |
2022 |
url |
https://hal.archives-ouvertes.fr/hal-03814771 https://hal.archives-ouvertes.fr/hal-03814771/document https://hal.archives-ouvertes.fr/hal-03814771/file/90674.pdf https://doi.org/10.1029/2021jc017696 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
ISSN: 2169-9275 EISSN: 2169-9291 Journal of Geophysical Research. Oceans https://hal.archives-ouvertes.fr/hal-03814771 Journal of Geophysical Research. Oceans, Wiley-Blackwell, 2022, 127 (1), pp.e2021JC017696. ⟨10.1029/2021jc017696⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2021jc017696 hal-03814771 https://hal.archives-ouvertes.fr/hal-03814771 https://hal.archives-ouvertes.fr/hal-03814771/document https://hal.archives-ouvertes.fr/hal-03814771/file/90674.pdf doi:10.1029/2021jc017696 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/2021jc017696 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
127 |
container_issue |
1 |
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1766132494189461504 |