Acquisition of isotopic composition for surface snow in East Antarctica and the links to climatic parameters

Abstract: The isotopic compositions of oxygen and hydrogen in ice cores are invaluable tools for the reconstruction of past climate variations. Used alone, they give insights into the variations of the local temperature, whereas taken together they can provide information on the climatic conditions...

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Main Author: celiaeschst
Format: Other/Unknown Material
Language:unknown
Published: AFEQ english 2017
Subjects:
East Antarctica
Antarc*
Antarctica
Online Access:http://afeqeng.hypotheses.org/512
id ftopenedition:oai:hypotheses.org:afeqeng/512
record_format openpolar
spelling ftopenedition:oai:hypotheses.org:afeqeng/512 2023-05-15T13:38:09+02:00 Acquisition of isotopic composition for surface snow in East Antarctica and the links to climatic parameters celiaeschst 2017-01-13T10:57:36Z http://afeqeng.hypotheses.org/512 unknown AFEQ english http://afeqeng.hypotheses.org/512 post 2017 ftopenedition 2017-03-08T16:20:36Z Abstract: The isotopic compositions of oxygen and hydrogen in ice cores are invaluable tools for the reconstruction of past climate variations. Used alone, they give insights into the variations of the local temperature, whereas taken together they can provide information on the climatic conditions at the point of origin of the moisture. However, recent analyses of snow from shallow pits indicate that the climatic signal can become erased in very low accumulation regions, due to local proces. Other/Unknown Material Antarc* Antarctica East Antarctica OpenEdition East Antarctica
institution Open Polar
collection OpenEdition
op_collection_id ftopenedition
language unknown
description Abstract: The isotopic compositions of oxygen and hydrogen in ice cores are invaluable tools for the reconstruction of past climate variations. Used alone, they give insights into the variations of the local temperature, whereas taken together they can provide information on the climatic conditions at the point of origin of the moisture. However, recent analyses of snow from shallow pits indicate that the climatic signal can become erased in very low accumulation regions, due to local proces.
format Other/Unknown Material
author celiaeschst
spellingShingle celiaeschst
Acquisition of isotopic composition for surface snow in East Antarctica and the links to climatic parameters
author_facet celiaeschst
author_sort celiaeschst
title Acquisition of isotopic composition for surface snow in East Antarctica and the links to climatic parameters
title_short Acquisition of isotopic composition for surface snow in East Antarctica and the links to climatic parameters
title_full Acquisition of isotopic composition for surface snow in East Antarctica and the links to climatic parameters
title_fullStr Acquisition of isotopic composition for surface snow in East Antarctica and the links to climatic parameters
title_full_unstemmed Acquisition of isotopic composition for surface snow in East Antarctica and the links to climatic parameters
title_sort acquisition of isotopic composition for surface snow in east antarctica and the links to climatic parameters
publisher AFEQ english
publishDate 2017
url http://afeqeng.hypotheses.org/512
geographic East Antarctica
geographic_facet East Antarctica
genre Antarc*
Antarctica
East Antarctica
genre_facet Antarc*
Antarctica
East Antarctica
op_relation http://afeqeng.hypotheses.org/512
_version_ 1766101994451238912

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