Surface studies of water isotopes in Antarctica for quantitative interpretation of deep ice core data

Polar ice cores are unique climate archives. Indeed, most of them have a continuous stratigraphy and present high temporal resolution of many climate variables in a single archive. While water isotopic records (dD or d18O) in ice cores are often taken as reference for past atmospheric temperature va...

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Main Author: celiaeschst
Format: Other/Unknown Material
Language:unknown
Published: AFEQ CNF-INQUA 2017
Subjects:
Antarc*
Antarctica
ice core
Online Access:http://afeq.hypotheses.org/1881
id ftopenedition:oai:hypotheses.org:afeq/1881
record_format openpolar
spelling ftopenedition:oai:hypotheses.org:afeq/1881 2023-05-15T13:58:45+02:00 Surface studies of water isotopes in Antarctica for quantitative interpretation of deep ice core data celiaeschst 2017-05-23T13:07:59Z http://afeq.hypotheses.org/1881 unknown AFEQ CNF-INQUA http://afeq.hypotheses.org/1881 post 2017 ftopenedition 2017-05-28T00:01:25Z Polar ice cores are unique climate archives. Indeed, most of them have a continuous stratigraphy and present high temporal resolution of many climate variables in a single archive. While water isotopic records (dD or d18O) in ice cores are often taken as reference for past atmospheric temperature variations, their relationship to temperature is associated with a large uncertainty. Several reasons are invoked to explain the limitation of such an approach; in particular, post-deposition effects. Other/Unknown Material Antarc* Antarctica ice core OpenEdition
institution Open Polar
collection OpenEdition
op_collection_id ftopenedition
language unknown
description Polar ice cores are unique climate archives. Indeed, most of them have a continuous stratigraphy and present high temporal resolution of many climate variables in a single archive. While water isotopic records (dD or d18O) in ice cores are often taken as reference for past atmospheric temperature variations, their relationship to temperature is associated with a large uncertainty. Several reasons are invoked to explain the limitation of such an approach; in particular, post-deposition effects.
format Other/Unknown Material
author celiaeschst
spellingShingle celiaeschst
Surface studies of water isotopes in Antarctica for quantitative interpretation of deep ice core data
author_facet celiaeschst
author_sort celiaeschst
title Surface studies of water isotopes in Antarctica for quantitative interpretation of deep ice core data
title_short Surface studies of water isotopes in Antarctica for quantitative interpretation of deep ice core data
title_full Surface studies of water isotopes in Antarctica for quantitative interpretation of deep ice core data
title_fullStr Surface studies of water isotopes in Antarctica for quantitative interpretation of deep ice core data
title_full_unstemmed Surface studies of water isotopes in Antarctica for quantitative interpretation of deep ice core data
title_sort surface studies of water isotopes in antarctica for quantitative interpretation of deep ice core data
publisher AFEQ CNF-INQUA
publishDate 2017
url http://afeq.hypotheses.org/1881
genre Antarc*
Antarctica
ice core
genre_facet Antarc*
Antarctica
ice core
op_relation http://afeq.hypotheses.org/1881
_version_ 1766267084535234560

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