id ftinsu:oai:HAL:hal-00409124v1
record_format openpolar
spelling ftinsu:oai:HAL:hal-00409124v1 2023-12-17T10:21:32+01:00 Present-day sea-level change: A review Nerem, R. S. Leuliette, E. Cazenave, A. 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) 2006 https://hal.science/hal-00409124 en eng HAL CCSD Elsevier hal-00409124 https://hal.science/hal-00409124 Comptes Rendus Géoscience https://hal.science/hal-00409124 Comptes Rendus Géoscience, 2006, 338 (14-15), pp.1077-1083 info:eu-repo/semantics/article Journal articles 2006 ftinsu 2023-11-22T17:27:40Z 1631-0713 Understanding of sea-level change has improved considerably over the last decade. Present-day knowledge of sea-level change is derived from tide gauge observations and satellite altimetry measurements. The average rate of sea-level change obtained from tide gauges over the last 50 years is +1.8 +/- 0.3 mm yr(-1). In comparison, altimeter measurements from TOPEX/Poseidon and Jason-1 have shown an average rise of +3.1 +/- 0.4 turn yr(-1) since 1993. It is not clear yet whether the larger rate of rise of the last decade reflects acceleration or decadal fluctuation. The causes of the present-day rate are a combination of increases in ocean temperatures and land ice melt from mountain glaciers, Greenland, and Antarctica. Regional variability in sea-level change, as evidenced by the quasi global coverage of altimeter satellites, appears dominated by non uniform change of thermal expansion. New satellite technologies, such as InSAR, ICESat, and GRACE make significant contributions to understanding sea-level change. Article in Journal/Newspaper Antarc* Antarctica Greenland Institut national des sciences de l'Univers: HAL-INSU Greenland
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
description 1631-0713 Understanding of sea-level change has improved considerably over the last decade. Present-day knowledge of sea-level change is derived from tide gauge observations and satellite altimetry measurements. The average rate of sea-level change obtained from tide gauges over the last 50 years is +1.8 +/- 0.3 mm yr(-1). In comparison, altimeter measurements from TOPEX/Poseidon and Jason-1 have shown an average rise of +3.1 +/- 0.4 turn yr(-1) since 1993. It is not clear yet whether the larger rate of rise of the last decade reflects acceleration or decadal fluctuation. The causes of the present-day rate are a combination of increases in ocean temperatures and land ice melt from mountain glaciers, Greenland, and Antarctica. Regional variability in sea-level change, as evidenced by the quasi global coverage of altimeter satellites, appears dominated by non uniform change of thermal expansion. New satellite technologies, such as InSAR, ICESat, and GRACE make significant contributions to understanding sea-level change.
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)
format Article in Journal/Newspaper
author Nerem, R. S.
Leuliette, E.
Cazenave, A.
spellingShingle Nerem, R. S.
Leuliette, E.
Cazenave, A.
Present-day sea-level change: A review
author_facet Nerem, R. S.
Leuliette, E.
Cazenave, A.
author_sort Nerem, R. S.
title Present-day sea-level change: A review
title_short Present-day sea-level change: A review
title_full Present-day sea-level change: A review
title_fullStr Present-day sea-level change: A review
title_full_unstemmed Present-day sea-level change: A review
title_sort present-day sea-level change: a review
publisher HAL CCSD
publishDate 2006
url https://hal.science/hal-00409124
geographic Greenland
geographic_facet Greenland
genre Antarc*
Antarctica
Greenland
genre_facet Antarc*
Antarctica
Greenland
op_source Comptes Rendus Géoscience
https://hal.science/hal-00409124
Comptes Rendus Géoscience, 2006, 338 (14-15), pp.1077-1083
op_relation hal-00409124
https://hal.science/hal-00409124
_version_ 1785535633004953600