Upper ocean variability between Iceland and Newfoundland, 1993-1998

International audience We investigate the variability of upper ocean temperature and surface salinity between Iceland and Newfoundland along World Ocean Circulation Experiment line AX2 in 1993-1998. North of 54°N, as well as close to Newfoundland, deviations from the seasonal cycle indicate upper oc...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Reverdin, Gilles, Verbrugge, Nathalie, Valdimarsson, Hedinn
Other Authors: Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Muséum national d'Histoire naturelle (MNHN)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 1999
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-00772190
https://hal.archives-ouvertes.fr/hal-00772190/document
https://hal.archives-ouvertes.fr/hal-00772190/file/98JC02713.pdf
https://doi.org/10.1029/1999JC900182
id ftccsdartic:oai:HAL:hal-00772190v1
record_format openpolar
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic Oceanography: Physical: Sea level variations
Oceanography: Physical: Hydrography
Oceanography: General: Climate and interannual variability
Meteorology and Atmospheric Dynamics: Ocean/atmosphere interactions
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]
[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
spellingShingle Oceanography: Physical: Sea level variations
Oceanography: Physical: Hydrography
Oceanography: General: Climate and interannual variability
Meteorology and Atmospheric Dynamics: Ocean/atmosphere interactions
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]
[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
Reverdin, Gilles
Verbrugge, Nathalie
Valdimarsson, Hedinn
Upper ocean variability between Iceland and Newfoundland, 1993-1998
topic_facet Oceanography: Physical: Sea level variations
Oceanography: Physical: Hydrography
Oceanography: General: Climate and interannual variability
Meteorology and Atmospheric Dynamics: Ocean/atmosphere interactions
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]
[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
description International audience We investigate the variability of upper ocean temperature and surface salinity between Iceland and Newfoundland along World Ocean Circulation Experiment line AX2 in 1993-1998. North of 54°N, as well as close to Newfoundland, deviations from the seasonal cycle indicate upper ocean warming from 1994 to 1998, with largest anomalous warming during late 1995/early 1996 and during the winter 1997/1998. North of 54°N, surface salinity increases after mid-1996. The winter of 1995/1996 is the first winter of weak westerlies after more than 20 years of strong westerly conditions in the subarctic gyre, and the ocean loses less heat during that winter than during a normal year. The magnitude of upper ocean heat content change is at least twice as large as what results from the change in air-sea fluxes, which indicates a complementary contribution to heat content change by advection. Altimetric sea level data indicate also an increase of sea level of the order of 6.5 cm during that year, out of which more than 4 cm is contributed by the steric change associated with the temperature increase. A principal component analysis of the sea level data suggests that the increase sensed along line AX2 west of the Reykjanes ridge is found in most of the subpolar gyre, although to a lesser extent in most other areas.
author2 Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN)
Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Muséum national d'Histoire naturelle (MNHN)-Institut Pierre-Simon-Laplace (IPSL (FR_636))
École normale supérieure - Paris (ENS Paris)
Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS Paris)
Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Reverdin, Gilles
Verbrugge, Nathalie
Valdimarsson, Hedinn
author_facet Reverdin, Gilles
Verbrugge, Nathalie
Valdimarsson, Hedinn
author_sort Reverdin, Gilles
title Upper ocean variability between Iceland and Newfoundland, 1993-1998
title_short Upper ocean variability between Iceland and Newfoundland, 1993-1998
title_full Upper ocean variability between Iceland and Newfoundland, 1993-1998
title_fullStr Upper ocean variability between Iceland and Newfoundland, 1993-1998
title_full_unstemmed Upper ocean variability between Iceland and Newfoundland, 1993-1998
title_sort upper ocean variability between iceland and newfoundland, 1993-1998
publisher HAL CCSD
publishDate 1999
url https://hal.archives-ouvertes.fr/hal-00772190
https://hal.archives-ouvertes.fr/hal-00772190/document
https://hal.archives-ouvertes.fr/hal-00772190/file/98JC02713.pdf
https://doi.org/10.1029/1999JC900182
long_lat ENVELOPE(-22.250,-22.250,65.467,65.467)
geographic Reykjanes
geographic_facet Reykjanes
genre Iceland
Newfoundland
Subarctic
genre_facet Iceland
Newfoundland
Subarctic
op_source ISSN: 0148-0227
EISSN: 2156-2202
Journal of Geophysical Research
https://hal.archives-ouvertes.fr/hal-00772190
Journal of Geophysical Research, American Geophysical Union, 1999, 104, pp.29599-29612. ⟨10.1029/1999JC900182⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/1999JC900182
hal-00772190
https://hal.archives-ouvertes.fr/hal-00772190
https://hal.archives-ouvertes.fr/hal-00772190/document
https://hal.archives-ouvertes.fr/hal-00772190/file/98JC02713.pdf
BIBCODE: 1999JGR.10429599R
doi:10.1029/1999JC900182
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1029/1999JC900182
container_title Journal of Geophysical Research: Oceans
container_volume 104
container_issue C12
container_start_page 29599
op_container_end_page 29611
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spelling ftccsdartic:oai:HAL:hal-00772190v1 2023-05-15T16:48:33+02:00 Upper ocean variability between Iceland and Newfoundland, 1993-1998 Reverdin, Gilles Verbrugge, Nathalie Valdimarsson, Hedinn Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Muséum national d'Histoire naturelle (MNHN)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) 1999 https://hal.archives-ouvertes.fr/hal-00772190 https://hal.archives-ouvertes.fr/hal-00772190/document https://hal.archives-ouvertes.fr/hal-00772190/file/98JC02713.pdf https://doi.org/10.1029/1999JC900182 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/1999JC900182 hal-00772190 https://hal.archives-ouvertes.fr/hal-00772190 https://hal.archives-ouvertes.fr/hal-00772190/document https://hal.archives-ouvertes.fr/hal-00772190/file/98JC02713.pdf BIBCODE: 1999JGR.10429599R doi:10.1029/1999JC900182 info:eu-repo/semantics/OpenAccess ISSN: 0148-0227 EISSN: 2156-2202 Journal of Geophysical Research https://hal.archives-ouvertes.fr/hal-00772190 Journal of Geophysical Research, American Geophysical Union, 1999, 104, pp.29599-29612. ⟨10.1029/1999JC900182⟩ Oceanography: Physical: Sea level variations Oceanography: Physical: Hydrography Oceanography: General: Climate and interannual variability Meteorology and Atmospheric Dynamics: Ocean/atmosphere interactions [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] info:eu-repo/semantics/article Journal articles 1999 ftccsdartic https://doi.org/10.1029/1999JC900182 2021-12-05T00:40:34Z International audience We investigate the variability of upper ocean temperature and surface salinity between Iceland and Newfoundland along World Ocean Circulation Experiment line AX2 in 1993-1998. North of 54°N, as well as close to Newfoundland, deviations from the seasonal cycle indicate upper ocean warming from 1994 to 1998, with largest anomalous warming during late 1995/early 1996 and during the winter 1997/1998. North of 54°N, surface salinity increases after mid-1996. The winter of 1995/1996 is the first winter of weak westerlies after more than 20 years of strong westerly conditions in the subarctic gyre, and the ocean loses less heat during that winter than during a normal year. The magnitude of upper ocean heat content change is at least twice as large as what results from the change in air-sea fluxes, which indicates a complementary contribution to heat content change by advection. Altimetric sea level data indicate also an increase of sea level of the order of 6.5 cm during that year, out of which more than 4 cm is contributed by the steric change associated with the temperature increase. A principal component analysis of the sea level data suggests that the increase sensed along line AX2 west of the Reykjanes ridge is found in most of the subpolar gyre, although to a lesser extent in most other areas. Article in Journal/Newspaper Iceland Newfoundland Subarctic Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Reykjanes ENVELOPE(-22.250,-22.250,65.467,65.467) Journal of Geophysical Research: Oceans 104 C12 29599 29611