Stable water isotopes of precipitation and firn cores from the northern Antarctic Peninsula region as a proxy for climate reconstruction

In order to investigate the climate variability in the northern Antarctic Peninsula region, this paper focuses on the relationship between stable isotope content of precipitation and firn, and main meteorological variables (air temperature, relative humidity, sea surface temperature, and sea ice ext...

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Published in:The Cryosphere
Main Authors: Fernandoy, F., Meyer, H., Tonelli, M.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2012
Subjects:
Online Access:https://doi.org/10.5194/tc-6-313-2012
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spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00026052 2023-05-15T13:36:44+02:00 Stable water isotopes of precipitation and firn cores from the northern Antarctic Peninsula region as a proxy for climate reconstruction Fernandoy, F. Meyer, H. Tonelli, M. 2012-03 electronic https://doi.org/10.5194/tc-6-313-2012 https://noa.gwlb.de/receive/cop_mods_00026052 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00026007/tc-6-313-2012.pdf https://tc.copernicus.org/articles/6/313/2012/tc-6-313-2012.pdf eng eng Copernicus Publications The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-6-313-2012 https://noa.gwlb.de/receive/cop_mods_00026052 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00026007/tc-6-313-2012.pdf https://tc.copernicus.org/articles/6/313/2012/tc-6-313-2012.pdf uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2012 ftnonlinearchiv https://doi.org/10.5194/tc-6-313-2012 2022-02-08T22:49:24Z In order to investigate the climate variability in the northern Antarctic Peninsula region, this paper focuses on the relationship between stable isotope content of precipitation and firn, and main meteorological variables (air temperature, relative humidity, sea surface temperature, and sea ice extent). Between 2008 and 2010, we collected precipitation samples and retrieved firn cores from several key sites in this region. We conclude that the deuterium excess oscillation represents a robust indicator of the meteorological variability on a seasonal to sub-seasonal scale. Low absolute deuterium excess values and the synchronous variation of both deuterium excess and air temperature imply that the evaporation of moisture occurs in the adjacent Southern Ocean. The δ18O-air temperature relationship is complicated and significant only at a (multi)seasonal scale. Backward trajectory calculations show that air-parcels arriving at the region during precipitation events predominantly originate at the South Pacific Ocean and Bellingshausen Sea. These investigations will be used as a calibration for ongoing and future research in the area, suggesting that appropriate locations for future ice core research are located above 600 m a.s.l. We selected the Plateau Laclavere, Antarctic Peninsula as the most promising site for a deeper drilling campaign. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Bellingshausen Sea ice core Sea ice Southern Ocean The Cryosphere Niedersächsisches Online-Archiv NOA Antarctic Antarctic Peninsula Bellingshausen Sea Pacific Southern Ocean The Cryosphere 6 2 313 330
institution Open Polar
collection Niedersächsisches Online-Archiv NOA
op_collection_id ftnonlinearchiv
language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Fernandoy, F.
Meyer, H.
Tonelli, M.
Stable water isotopes of precipitation and firn cores from the northern Antarctic Peninsula region as a proxy for climate reconstruction
topic_facet article
Verlagsveröffentlichung
description In order to investigate the climate variability in the northern Antarctic Peninsula region, this paper focuses on the relationship between stable isotope content of precipitation and firn, and main meteorological variables (air temperature, relative humidity, sea surface temperature, and sea ice extent). Between 2008 and 2010, we collected precipitation samples and retrieved firn cores from several key sites in this region. We conclude that the deuterium excess oscillation represents a robust indicator of the meteorological variability on a seasonal to sub-seasonal scale. Low absolute deuterium excess values and the synchronous variation of both deuterium excess and air temperature imply that the evaporation of moisture occurs in the adjacent Southern Ocean. The δ18O-air temperature relationship is complicated and significant only at a (multi)seasonal scale. Backward trajectory calculations show that air-parcels arriving at the region during precipitation events predominantly originate at the South Pacific Ocean and Bellingshausen Sea. These investigations will be used as a calibration for ongoing and future research in the area, suggesting that appropriate locations for future ice core research are located above 600 m a.s.l. We selected the Plateau Laclavere, Antarctic Peninsula as the most promising site for a deeper drilling campaign.
format Article in Journal/Newspaper
author Fernandoy, F.
Meyer, H.
Tonelli, M.
author_facet Fernandoy, F.
Meyer, H.
Tonelli, M.
author_sort Fernandoy, F.
title Stable water isotopes of precipitation and firn cores from the northern Antarctic Peninsula region as a proxy for climate reconstruction
title_short Stable water isotopes of precipitation and firn cores from the northern Antarctic Peninsula region as a proxy for climate reconstruction
title_full Stable water isotopes of precipitation and firn cores from the northern Antarctic Peninsula region as a proxy for climate reconstruction
title_fullStr Stable water isotopes of precipitation and firn cores from the northern Antarctic Peninsula region as a proxy for climate reconstruction
title_full_unstemmed Stable water isotopes of precipitation and firn cores from the northern Antarctic Peninsula region as a proxy for climate reconstruction
title_sort stable water isotopes of precipitation and firn cores from the northern antarctic peninsula region as a proxy for climate reconstruction
publisher Copernicus Publications
publishDate 2012
url https://doi.org/10.5194/tc-6-313-2012
https://noa.gwlb.de/receive/cop_mods_00026052
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00026007/tc-6-313-2012.pdf
https://tc.copernicus.org/articles/6/313/2012/tc-6-313-2012.pdf
geographic Antarctic
Antarctic Peninsula
Bellingshausen Sea
Pacific
Southern Ocean
geographic_facet Antarctic
Antarctic Peninsula
Bellingshausen Sea
Pacific
Southern Ocean
genre Antarc*
Antarctic
Antarctic Peninsula
Bellingshausen Sea
ice core
Sea ice
Southern Ocean
The Cryosphere
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Bellingshausen Sea
ice core
Sea ice
Southern Ocean
The Cryosphere
op_relation The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424
https://doi.org/10.5194/tc-6-313-2012
https://noa.gwlb.de/receive/cop_mods_00026052
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00026007/tc-6-313-2012.pdf
https://tc.copernicus.org/articles/6/313/2012/tc-6-313-2012.pdf
op_rights uneingeschränkt
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/tc-6-313-2012
container_title The Cryosphere
container_volume 6
container_issue 2
container_start_page 313
op_container_end_page 330
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