Atmospheric Moisture Transport to the Arctic: Assessment of Reanalyses and Analysis of Transport Components

International audience The atmospheric water cycle of the Arctic is evaluated via seven global reanalyses and in radiosonde observations covering the 1979–2013 period. In the regional moisture budget, evaporation and precipitation are the least consistent terms among different datasets. Despite the...

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Published in:Journal of Climate
Main Authors: Dufour, Ambroise, Zolina, Olga, Gulev, Sergei K.
Other Authors: Laboratoire de glaciologie et géophysique de l'environnement (LGGE), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG ), Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 )-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ), Shirshov Institut of Oceanography, Russian Academy of Sciences Moscow (RAS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2016
Subjects:
Online Access:https://insu.hal.science/insu-01388439
https://insu.hal.science/insu-01388439/document
https://insu.hal.science/insu-01388439/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20Atmospheric%20Moisture%20Transport%20to%20the%20Arctic%20Assessment%20of%20Reanalyses%20and%20Analysis%20of%20Transport%20Components.pdf
https://doi.org/10.1175/JCLI-D-15-0559.1
id ftinsu:oai:HAL:insu-01388439v1
record_format openpolar
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic Geographic location/entity
Arctic
Circulation/ Dynamics
Hydrologic cycle
Transport
Observational techniques and algorithms
Radiosonde observations
Models and modeling
Reanalysis data
[SDE]Environmental Sciences
spellingShingle Geographic location/entity
Arctic
Circulation/ Dynamics
Hydrologic cycle
Transport
Observational techniques and algorithms
Radiosonde observations
Models and modeling
Reanalysis data
[SDE]Environmental Sciences
Dufour, Ambroise
Zolina, Olga
Gulev, Sergei K.
Atmospheric Moisture Transport to the Arctic: Assessment of Reanalyses and Analysis of Transport Components
topic_facet Geographic location/entity
Arctic
Circulation/ Dynamics
Hydrologic cycle
Transport
Observational techniques and algorithms
Radiosonde observations
Models and modeling
Reanalysis data
[SDE]Environmental Sciences
description International audience The atmospheric water cycle of the Arctic is evaluated via seven global reanalyses and in radiosonde observations covering the 1979–2013 period. In the regional moisture budget, evaporation and precipitation are the least consistent terms among different datasets. Despite the assimilation of radiosoundings, the reanalyses present a tendency to overestimate the moisture transport. Aside from this overestimation, the reanalyses exhibit a remarkable agreement with the radiosondes in terms of spatial and temporal patterns. The northern North Atlantic, subpolar North Pacific, and Labrador Sea stand out as the main gateways for moisture to the Arctic in all reanalyses. Because these regions correspond to the end of the storm tracks, the link between moisture transports and extratropical cyclones is further investigated by decomposing the moisture fluxes in the mean flow and transient eddy parts. In all reanalyses, the former term tends to cancel out when averaged over a latitude circle, leaving the latter to provide the bulk of the midlatitude moisture imports (89%–94% at 70°N). Although the Arctic warms faster than the rest of the world, the impact of these changes on its water cycle remains ambiguous. In most datasets, evaporation, precipitation, and precipitable water increase in line with what is expected from a warming signal. At the same time, the moisture transports have decreased in all the reanalyses but not in the radiosonde observations, though none of these trends is statistically significant. The fluxes do not scale with the Clausius–Clapeyron relation because the increasing humidity is not correlated with the meridional wind, particularly near the surface.
author2 Laboratoire de glaciologie et géophysique de l'environnement (LGGE)
Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG )
Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 )-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 )
Shirshov Institut of Oceanography
Russian Academy of Sciences Moscow (RAS)
format Article in Journal/Newspaper
author Dufour, Ambroise
Zolina, Olga
Gulev, Sergei K.
author_facet Dufour, Ambroise
Zolina, Olga
Gulev, Sergei K.
author_sort Dufour, Ambroise
title Atmospheric Moisture Transport to the Arctic: Assessment of Reanalyses and Analysis of Transport Components
title_short Atmospheric Moisture Transport to the Arctic: Assessment of Reanalyses and Analysis of Transport Components
title_full Atmospheric Moisture Transport to the Arctic: Assessment of Reanalyses and Analysis of Transport Components
title_fullStr Atmospheric Moisture Transport to the Arctic: Assessment of Reanalyses and Analysis of Transport Components
title_full_unstemmed Atmospheric Moisture Transport to the Arctic: Assessment of Reanalyses and Analysis of Transport Components
title_sort atmospheric moisture transport to the arctic: assessment of reanalyses and analysis of transport components
publisher HAL CCSD
publishDate 2016
url https://insu.hal.science/insu-01388439
https://insu.hal.science/insu-01388439/document
https://insu.hal.science/insu-01388439/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20Atmospheric%20Moisture%20Transport%20to%20the%20Arctic%20Assessment%20of%20Reanalyses%20and%20Analysis%20of%20Transport%20Components.pdf
https://doi.org/10.1175/JCLI-D-15-0559.1
genre Arctic
Labrador Sea
North Atlantic
genre_facet Arctic
Labrador Sea
North Atlantic
op_source ISSN: 0894-8755
EISSN: 1520-0442
Journal of Climate
https://insu.hal.science/insu-01388439
Journal of Climate, 2016, 29 (14), pp.5061-5081. ⟨10.1175/JCLI-D-15-0559.1⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1175/JCLI-D-15-0559.1
insu-01388439
https://insu.hal.science/insu-01388439
https://insu.hal.science/insu-01388439/document
https://insu.hal.science/insu-01388439/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20Atmospheric%20Moisture%20Transport%20to%20the%20Arctic%20Assessment%20of%20Reanalyses%20and%20Analysis%20of%20Transport%20Components.pdf
doi:10.1175/JCLI-D-15-0559.1
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1175/JCLI-D-15-0559.1
container_title Journal of Climate
container_volume 29
container_issue 14
container_start_page 5061
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spelling ftinsu:oai:HAL:insu-01388439v1 2024-04-28T08:07:30+00:00 Atmospheric Moisture Transport to the Arctic: Assessment of Reanalyses and Analysis of Transport Components Dufour, Ambroise Zolina, Olga Gulev, Sergei K. Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Observatoire des Sciences de l'Univers de Grenoble (OSUG ) Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 )-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ) Shirshov Institut of Oceanography Russian Academy of Sciences Moscow (RAS) 2016-06 https://insu.hal.science/insu-01388439 https://insu.hal.science/insu-01388439/document https://insu.hal.science/insu-01388439/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20Atmospheric%20Moisture%20Transport%20to%20the%20Arctic%20Assessment%20of%20Reanalyses%20and%20Analysis%20of%20Transport%20Components.pdf https://doi.org/10.1175/JCLI-D-15-0559.1 en eng HAL CCSD American Meteorological Society info:eu-repo/semantics/altIdentifier/doi/10.1175/JCLI-D-15-0559.1 insu-01388439 https://insu.hal.science/insu-01388439 https://insu.hal.science/insu-01388439/document https://insu.hal.science/insu-01388439/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20Atmospheric%20Moisture%20Transport%20to%20the%20Arctic%20Assessment%20of%20Reanalyses%20and%20Analysis%20of%20Transport%20Components.pdf doi:10.1175/JCLI-D-15-0559.1 info:eu-repo/semantics/OpenAccess ISSN: 0894-8755 EISSN: 1520-0442 Journal of Climate https://insu.hal.science/insu-01388439 Journal of Climate, 2016, 29 (14), pp.5061-5081. ⟨10.1175/JCLI-D-15-0559.1⟩ Geographic location/entity Arctic Circulation/ Dynamics Hydrologic cycle Transport Observational techniques and algorithms Radiosonde observations Models and modeling Reanalysis data [SDE]Environmental Sciences info:eu-repo/semantics/article Journal articles 2016 ftinsu https://doi.org/10.1175/JCLI-D-15-0559.1 2024-04-05T00:38:11Z International audience The atmospheric water cycle of the Arctic is evaluated via seven global reanalyses and in radiosonde observations covering the 1979–2013 period. In the regional moisture budget, evaporation and precipitation are the least consistent terms among different datasets. Despite the assimilation of radiosoundings, the reanalyses present a tendency to overestimate the moisture transport. Aside from this overestimation, the reanalyses exhibit a remarkable agreement with the radiosondes in terms of spatial and temporal patterns. The northern North Atlantic, subpolar North Pacific, and Labrador Sea stand out as the main gateways for moisture to the Arctic in all reanalyses. Because these regions correspond to the end of the storm tracks, the link between moisture transports and extratropical cyclones is further investigated by decomposing the moisture fluxes in the mean flow and transient eddy parts. In all reanalyses, the former term tends to cancel out when averaged over a latitude circle, leaving the latter to provide the bulk of the midlatitude moisture imports (89%–94% at 70°N). Although the Arctic warms faster than the rest of the world, the impact of these changes on its water cycle remains ambiguous. In most datasets, evaporation, precipitation, and precipitable water increase in line with what is expected from a warming signal. At the same time, the moisture transports have decreased in all the reanalyses but not in the radiosonde observations, though none of these trends is statistically significant. The fluxes do not scale with the Clausius–Clapeyron relation because the increasing humidity is not correlated with the meridional wind, particularly near the surface. Article in Journal/Newspaper Arctic Labrador Sea North Atlantic Institut national des sciences de l'Univers: HAL-INSU Journal of Climate 29 14 5061 5081