A new pattern of the moisture transport for precipitation related to the drastic decline in Arctic sea ice extent

In this study we use the term moisture transport for precipitation for a target region as the moisture coming to this region from its major moisture sources resulting in precipitation over the target region (MTP). We have identified changes in the pattern of moisture transport for precipitation...

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Main Authors: L. Gimeno-Sotelo, R. Nieto, M. Vázquez, L. Gimeno
Format: Article
Language:English
Published: Copernicus Publications 2018-05-01
Series:Earth System Dynamics
Online Access:https://www.earth-syst-dynam.net/9/611/2018/esd-9-611-2018.pdf
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spelling doaj-809d0b680ce24a22acf88e30b96322652020-11-24T22:26:04ZengCopernicus PublicationsEarth System Dynamics2190-49792190-49872018-05-01961162510.5194/esd-9-611-2018A new pattern of the moisture transport for precipitation related to the drastic decline in Arctic sea ice extentL. Gimeno-Sotelo0R. Nieto1M. Vázquez2L. Gimeno3Facultade de Matemáticas, Universidade de Santiago de Compostela, Santiago de Compostela, 15782 SpainEnvironmental Physics Laboratory (EphysLab), Universidade de Vigo, Ourense, 32004, SpainEnvironmental Physics Laboratory (EphysLab), Universidade de Vigo, Ourense, 32004, SpainEnvironmental Physics Laboratory (EphysLab), Universidade de Vigo, Ourense, 32004, SpainIn this study we use the term moisture transport for precipitation for a target region as the moisture coming to this region from its major moisture sources resulting in precipitation over the target region (MTP). We have identified changes in the pattern of moisture transport for precipitation over the Arctic region, the Arctic Ocean, and its 13 main subdomains concurrent with the major sea ice decline that occurred in 2003. The pattern consists of a general decrease in moisture transport in summer and enhanced moisture transport in autumn and early winter, with different contributions depending on the moisture source and ocean subregion. The pattern is statistically significant and consistent with changes in the vertically integrated moisture fluxes and frequency of circulation types. The results of this paper also reveal that the assumed and partially documented enhanced poleward moisture transport from lower latitudes as a consequence of increased moisture from climate change seems to be less simple and constant than typically recognised in relation to enhanced Arctic precipitation throughout the year in the present climate.https://www.earth-syst-dynam.net/9/611/2018/esd-9-611-2018.pdf
collection DOAJ
language English
format Article
sources DOAJ
author L. Gimeno-Sotelo
R. Nieto
M. Vázquez
L. Gimeno
spellingShingle L. Gimeno-Sotelo
R. Nieto
M. Vázquez
L. Gimeno
A new pattern of the moisture transport for precipitation related to the drastic decline in Arctic sea ice extent
Earth System Dynamics
author_facet L. Gimeno-Sotelo
R. Nieto
M. Vázquez
L. Gimeno
author_sort L. Gimeno-Sotelo
title A new pattern of the moisture transport for precipitation related to the drastic decline in Arctic sea ice extent
title_short A new pattern of the moisture transport for precipitation related to the drastic decline in Arctic sea ice extent
title_full A new pattern of the moisture transport for precipitation related to the drastic decline in Arctic sea ice extent
title_fullStr A new pattern of the moisture transport for precipitation related to the drastic decline in Arctic sea ice extent
title_full_unstemmed A new pattern of the moisture transport for precipitation related to the drastic decline in Arctic sea ice extent
title_sort new pattern of the moisture transport for precipitation related to the drastic decline in arctic sea ice extent
publisher Copernicus Publications
series Earth System Dynamics
issn 2190-4979
2190-4987
publishDate 2018-05-01
description In this study we use the term moisture transport for precipitation for a target region as the moisture coming to this region from its major moisture sources resulting in precipitation over the target region (MTP). We have identified changes in the pattern of moisture transport for precipitation over the Arctic region, the Arctic Ocean, and its 13 main subdomains concurrent with the major sea ice decline that occurred in 2003. The pattern consists of a general decrease in moisture transport in summer and enhanced moisture transport in autumn and early winter, with different contributions depending on the moisture source and ocean subregion. The pattern is statistically significant and consistent with changes in the vertically integrated moisture fluxes and frequency of circulation types. The results of this paper also reveal that the assumed and partially documented enhanced poleward moisture transport from lower latitudes as a consequence of increased moisture from climate change seems to be less simple and constant than typically recognised in relation to enhanced Arctic precipitation throughout the year in the present climate.
url https://www.earth-syst-dynam.net/9/611/2018/esd-9-611-2018.pdf
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