A 4.5 Year‐Long Record of Svalbard Water Vapor Isotopic Composition Documents Winter Air Mass Origin
International audience From May 2014 to September 2018, a laser spectrometer analyzer provided a 4.5 years continuous record of water vapor isotopic composition at Ny‐Ålesund (8 m above sea level, a.s.l.), Svalbard. It corresponds to the longest data set published in polar regions. A comparison of t...
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Online Access: | https://hal.science/hal-03087623 https://hal.science/hal-03087623/document https://hal.science/hal-03087623/file/Main_manuscript_final.pdf https://doi.org/10.1029/2020JD032681 |
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ftinsu:oai:HAL:hal-03087623v1 2024-04-28T08:08:42+00:00 A 4.5 Year‐Long Record of Svalbard Water Vapor Isotopic Composition Documents Winter Air Mass Origin Leroy‐dos Santos, C. Masson‐delmotte, V. Casado, M. Fourré, E. Steen‐larsen, H. Maturilli, M. Orsi, A. Berchet, A. Cattani, O. Minster, B. Gherardi, J. Landais, A. Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Alfred Wegener Institute for Polar and Marine Research (AWI) Geophysical Institute Bergen (GFI / BiU) University of Bergen (UiB) 2020-12-16 https://hal.science/hal-03087623 https://hal.science/hal-03087623/document https://hal.science/hal-03087623/file/Main_manuscript_final.pdf https://doi.org/10.1029/2020JD032681 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2020JD032681 hal-03087623 https://hal.science/hal-03087623 https://hal.science/hal-03087623/document https://hal.science/hal-03087623/file/Main_manuscript_final.pdf doi:10.1029/2020JD032681 info:eu-repo/semantics/OpenAccess ISSN: 2169-897X EISSN: 2169-8996 Journal of Geophysical Research: Atmospheres https://hal.science/hal-03087623 Journal of Geophysical Research: Atmospheres, 2020, 125 (23), ⟨10.1029/2020JD032681⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2020 ftinsu https://doi.org/10.1029/2020JD032681 2024-04-05T00:38:11Z International audience From May 2014 to September 2018, a laser spectrometer analyzer provided a 4.5 years continuous record of water vapor isotopic composition at Ny‐Ålesund (8 m above sea level, a.s.l.), Svalbard. It corresponds to the longest data set published in polar regions. A comparison of this data set with a parallel similar data set obtained during 20 days by a second laser spectrometer installed near Mount Zeppelin (474 m a.s.l.) shows that this data set is representative of a regional signal. In addition, the observation of insignificant diurnal cycles in the isotopic signal compared to the strong isotopic signature of synoptic events and the comparison of simultaneous measurements in the vapor and in rain or snow samples lead to the conclusion that our record reflects a large part of the regional dynamics of the atmospheric water cycle driven by large‐scale variability. This study focuses on winters dominated by the occurrence of synoptic events associated with humidity peaks. Using statistics and back trajectories calculations, we link high humidity peaks characterized by an anticorrelation between δ18O and d‐excess in the water vapor to a rapid shift of air mass source regions from the Arctic to the North Atlantic Ocean below 60°N. On the other hand, correlation between δ18O and d‐excess may be associated with a shift of air mass sources within the Arctic. These results demonstrate the added value of long‐term water vapor isotopic monitoring to better understand the moisture origin in the Arctic and the atmospheric dynamics. Article in Journal/Newspaper Arctic North Atlantic Ny Ålesund Ny-Ålesund Svalbard Institut national des sciences de l'Univers: HAL-INSU Journal of Geophysical Research: Atmospheres 125 23 |
institution |
Open Polar |
collection |
Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
spellingShingle |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment Leroy‐dos Santos, C. Masson‐delmotte, V. Casado, M. Fourré, E. Steen‐larsen, H. Maturilli, M. Orsi, A. Berchet, A. Cattani, O. Minster, B. Gherardi, J. Landais, A. A 4.5 Year‐Long Record of Svalbard Water Vapor Isotopic Composition Documents Winter Air Mass Origin |
topic_facet |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
description |
International audience From May 2014 to September 2018, a laser spectrometer analyzer provided a 4.5 years continuous record of water vapor isotopic composition at Ny‐Ålesund (8 m above sea level, a.s.l.), Svalbard. It corresponds to the longest data set published in polar regions. A comparison of this data set with a parallel similar data set obtained during 20 days by a second laser spectrometer installed near Mount Zeppelin (474 m a.s.l.) shows that this data set is representative of a regional signal. In addition, the observation of insignificant diurnal cycles in the isotopic signal compared to the strong isotopic signature of synoptic events and the comparison of simultaneous measurements in the vapor and in rain or snow samples lead to the conclusion that our record reflects a large part of the regional dynamics of the atmospheric water cycle driven by large‐scale variability. This study focuses on winters dominated by the occurrence of synoptic events associated with humidity peaks. Using statistics and back trajectories calculations, we link high humidity peaks characterized by an anticorrelation between δ18O and d‐excess in the water vapor to a rapid shift of air mass source regions from the Arctic to the North Atlantic Ocean below 60°N. On the other hand, correlation between δ18O and d‐excess may be associated with a shift of air mass sources within the Arctic. These results demonstrate the added value of long‐term water vapor isotopic monitoring to better understand the moisture origin in the Arctic and the atmospheric dynamics. |
author2 |
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Alfred Wegener Institute for Polar and Marine Research (AWI) Geophysical Institute Bergen (GFI / BiU) University of Bergen (UiB) |
format |
Article in Journal/Newspaper |
author |
Leroy‐dos Santos, C. Masson‐delmotte, V. Casado, M. Fourré, E. Steen‐larsen, H. Maturilli, M. Orsi, A. Berchet, A. Cattani, O. Minster, B. Gherardi, J. Landais, A. |
author_facet |
Leroy‐dos Santos, C. Masson‐delmotte, V. Casado, M. Fourré, E. Steen‐larsen, H. Maturilli, M. Orsi, A. Berchet, A. Cattani, O. Minster, B. Gherardi, J. Landais, A. |
author_sort |
Leroy‐dos Santos, C. |
title |
A 4.5 Year‐Long Record of Svalbard Water Vapor Isotopic Composition Documents Winter Air Mass Origin |
title_short |
A 4.5 Year‐Long Record of Svalbard Water Vapor Isotopic Composition Documents Winter Air Mass Origin |
title_full |
A 4.5 Year‐Long Record of Svalbard Water Vapor Isotopic Composition Documents Winter Air Mass Origin |
title_fullStr |
A 4.5 Year‐Long Record of Svalbard Water Vapor Isotopic Composition Documents Winter Air Mass Origin |
title_full_unstemmed |
A 4.5 Year‐Long Record of Svalbard Water Vapor Isotopic Composition Documents Winter Air Mass Origin |
title_sort |
4.5 year‐long record of svalbard water vapor isotopic composition documents winter air mass origin |
publisher |
HAL CCSD |
publishDate |
2020 |
url |
https://hal.science/hal-03087623 https://hal.science/hal-03087623/document https://hal.science/hal-03087623/file/Main_manuscript_final.pdf https://doi.org/10.1029/2020JD032681 |
genre |
Arctic North Atlantic Ny Ålesund Ny-Ålesund Svalbard |
genre_facet |
Arctic North Atlantic Ny Ålesund Ny-Ålesund Svalbard |
op_source |
ISSN: 2169-897X EISSN: 2169-8996 Journal of Geophysical Research: Atmospheres https://hal.science/hal-03087623 Journal of Geophysical Research: Atmospheres, 2020, 125 (23), ⟨10.1029/2020JD032681⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2020JD032681 hal-03087623 https://hal.science/hal-03087623 https://hal.science/hal-03087623/document https://hal.science/hal-03087623/file/Main_manuscript_final.pdf doi:10.1029/2020JD032681 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/2020JD032681 |
container_title |
Journal of Geophysical Research: Atmospheres |
container_volume |
125 |
container_issue |
23 |
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1797577368109318144 |