Forced and chaotic interannual variability of regional sea level and its components over 1993-2015
International audience Since the 1990s, satellite altimetry has become the main observing system for continuously measuring the sea level variations with a near global coverage, revealing a global mean sea level rise of 3.3 mm/yr since 1993 with large regional sea level variability. These measuremen...
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Language: | English |
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HAL CCSD
2020
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Online Access: | https://hal.science/hal-04549924 |
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ftunivbrest:oai:HAL:hal-04549924v1 |
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openpolar |
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Open Polar |
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Université de Bretagne Occidentale: HAL |
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ftunivbrest |
language |
English |
topic |
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography |
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[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography Carret, Alice Llovel, W. Penduff, Thierry Molines, Jean-Marc Forced and chaotic interannual variability of regional sea level and its components over 1993-2015 |
topic_facet |
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography |
description |
International audience Since the 1990s, satellite altimetry has become the main observing system for continuously measuring the sea level variations with a near global coverage, revealing a global mean sea level rise of 3.3 mm/yr since 1993 with large regional sea level variability. These measurements highlight complex structures especially for the western boundary currents or the Antarctic Circumpolar Current. A recent study shows that the chaotic ocean variability may mask atmospherically-forced regional sea level trends over 38% of the global ocean area from 1993 to 2015. The present study aims to complement this work in focusing on the interannual variability of regional sea level, which can show huge variations occurring in addition to the sea level trends. A global ¼° ocean/sea-ice 50-member ensemble simulation is considered to disentangle the imprints of the atmospheric forcing and the chaotic ocean variability on the interannual variability of regional sea level and its causes (i.e., steric sea level and manometric sea level contribution) over 1993-2015. First it is validated against observations. On the contrary to previous studies, we demonstrated that the forced signal has a signature for scales smaller than 3x3° and can be important in the western boundary current. The forced and chaotic interannual variability mainly have a steric origin except in coastal areas. However in the ACC, the chaotic variability is strong for both the steric and manometric contributions. Finally this study quantifies to what extent the chaotic variability explains the total interannual variability, questioning its detection and its characterisation. |
author2 |
Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) 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) Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université Grenoble Alpes (UGA) |
format |
Conference Object |
author |
Carret, Alice Llovel, W. Penduff, Thierry Molines, Jean-Marc |
author_facet |
Carret, Alice Llovel, W. Penduff, Thierry Molines, Jean-Marc |
author_sort |
Carret, Alice |
title |
Forced and chaotic interannual variability of regional sea level and its components over 1993-2015 |
title_short |
Forced and chaotic interannual variability of regional sea level and its components over 1993-2015 |
title_full |
Forced and chaotic interannual variability of regional sea level and its components over 1993-2015 |
title_fullStr |
Forced and chaotic interannual variability of regional sea level and its components over 1993-2015 |
title_full_unstemmed |
Forced and chaotic interannual variability of regional sea level and its components over 1993-2015 |
title_sort |
forced and chaotic interannual variability of regional sea level and its components over 1993-2015 |
publisher |
HAL CCSD |
publishDate |
2020 |
url |
https://hal.science/hal-04549924 |
op_coverage |
Online, United States |
genre |
Antarc* Antarctic Sea ice |
genre_facet |
Antarc* Antarctic Sea ice |
op_source |
Ocean Surface Topography Science Team Meeting (OSTST 2020) https://hal.science/hal-04549924 Ocean Surface Topography Science Team Meeting (OSTST 2020), Oct 2020, Online, United States https://sealevel.jpl.nasa.gov/events/23/ostst-2020-virtual-meetiing/ |
op_relation |
hal-04549924 https://hal.science/hal-04549924 |
_version_ |
1799470367174033408 |
spelling |
ftunivbrest:oai:HAL:hal-04549924v1 2024-05-19T07:32:21+00:00 Forced and chaotic interannual variability of regional sea level and its components over 1993-2015 Carret, Alice Llovel, W. Penduff, Thierry Molines, Jean-Marc Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) 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) Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université Grenoble Alpes (UGA) Online, United States 2020-10-19 https://hal.science/hal-04549924 en eng HAL CCSD hal-04549924 https://hal.science/hal-04549924 Ocean Surface Topography Science Team Meeting (OSTST 2020) https://hal.science/hal-04549924 Ocean Surface Topography Science Team Meeting (OSTST 2020), Oct 2020, Online, United States https://sealevel.jpl.nasa.gov/events/23/ostst-2020-virtual-meetiing/ [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography info:eu-repo/semantics/conferenceObject Conference papers 2020 ftunivbrest 2024-04-25T15:55:19Z International audience Since the 1990s, satellite altimetry has become the main observing system for continuously measuring the sea level variations with a near global coverage, revealing a global mean sea level rise of 3.3 mm/yr since 1993 with large regional sea level variability. These measurements highlight complex structures especially for the western boundary currents or the Antarctic Circumpolar Current. A recent study shows that the chaotic ocean variability may mask atmospherically-forced regional sea level trends over 38% of the global ocean area from 1993 to 2015. The present study aims to complement this work in focusing on the interannual variability of regional sea level, which can show huge variations occurring in addition to the sea level trends. A global ¼° ocean/sea-ice 50-member ensemble simulation is considered to disentangle the imprints of the atmospheric forcing and the chaotic ocean variability on the interannual variability of regional sea level and its causes (i.e., steric sea level and manometric sea level contribution) over 1993-2015. First it is validated against observations. On the contrary to previous studies, we demonstrated that the forced signal has a signature for scales smaller than 3x3° and can be important in the western boundary current. The forced and chaotic interannual variability mainly have a steric origin except in coastal areas. However in the ACC, the chaotic variability is strong for both the steric and manometric contributions. Finally this study quantifies to what extent the chaotic variability explains the total interannual variability, questioning its detection and its characterisation. Conference Object Antarc* Antarctic Sea ice Université de Bretagne Occidentale: HAL |