High resolution stable water isotope composition (δ¹⁸O and dD) of three firn cores and on precipitation from O'Higgins Station, Antarctica, 2008-2009 ...

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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Main Authors: Fernandoy, Francisco, Meyer, Hanno, Tonelli, Marco
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2012
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.871080
https://doi.pangaea.de/10.1594/PANGAEA.871080
id ftdatacite:10.1594/pangaea.871080
record_format openpolar
spelling ftdatacite:10.1594/pangaea.871080 2024-09-15T17:45:31+00:00 High resolution stable water isotope composition (δ¹⁸O and dD) of three firn cores and on precipitation from O'Higgins Station, Antarctica, 2008-2009 ... Fernandoy, Francisco Meyer, Hanno Tonelli, Marco 2012 application/zip https://dx.doi.org/10.1594/pangaea.871080 https://doi.pangaea.de/10.1594/PANGAEA.871080 en eng PANGAEA https://dx.doi.org/10.5194/tc-6-313-2012 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 article Collection Supplementary Publication Series of Datasets 2012 ftdatacite https://doi.org/10.1594/pangaea.87108010.5194/tc-6-313-2012 2024-08-01T11:01:20Z 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 d18O-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 ... : Supplement to: Fernandoy, Francisco; Meyer, Hanno; Tonelli, Marco (2012): Stable water isotopes of precipitation and firn cores from the northern Antarctic Peninsula region as a proxy for climate reconstruction. The Cryosphere, 6(2), 313-330 ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica Sea ice Southern Ocean DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
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 d18O-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 ... : Supplement to: Fernandoy, Francisco; Meyer, Hanno; Tonelli, Marco (2012): Stable water isotopes of precipitation and firn cores from the northern Antarctic Peninsula region as a proxy for climate reconstruction. The Cryosphere, 6(2), 313-330 ...
format Article in Journal/Newspaper
author Fernandoy, Francisco
Meyer, Hanno
Tonelli, Marco
spellingShingle Fernandoy, Francisco
Meyer, Hanno
Tonelli, Marco
High resolution stable water isotope composition (δ¹⁸O and dD) of three firn cores and on precipitation from O'Higgins Station, Antarctica, 2008-2009 ...
author_facet Fernandoy, Francisco
Meyer, Hanno
Tonelli, Marco
author_sort Fernandoy, Francisco
title High resolution stable water isotope composition (δ¹⁸O and dD) of three firn cores and on precipitation from O'Higgins Station, Antarctica, 2008-2009 ...
title_short High resolution stable water isotope composition (δ¹⁸O and dD) of three firn cores and on precipitation from O'Higgins Station, Antarctica, 2008-2009 ...
title_full High resolution stable water isotope composition (δ¹⁸O and dD) of three firn cores and on precipitation from O'Higgins Station, Antarctica, 2008-2009 ...
title_fullStr High resolution stable water isotope composition (δ¹⁸O and dD) of three firn cores and on precipitation from O'Higgins Station, Antarctica, 2008-2009 ...
title_full_unstemmed High resolution stable water isotope composition (δ¹⁸O and dD) of three firn cores and on precipitation from O'Higgins Station, Antarctica, 2008-2009 ...
title_sort high resolution stable water isotope composition (δ¹⁸o and dd) of three firn cores and on precipitation from o'higgins station, antarctica, 2008-2009 ...
publisher PANGAEA
publishDate 2012
url https://dx.doi.org/10.1594/pangaea.871080
https://doi.pangaea.de/10.1594/PANGAEA.871080
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Sea ice
Southern Ocean
op_relation https://dx.doi.org/10.5194/tc-6-313-2012
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.87108010.5194/tc-6-313-2012
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