ECHAM5-wiso simulation data for Antarctica

Stable water isotope records from Antarctica are key for our understanding of Quaternary climate variations. However, the exact quantitative interpretation of these important climate proxy records in terms of surface temperature, ice sheet height and other climatic changes is still a matter of debat...

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Main Authors: Werner, Martin, Jouzel, Jean, Masson-Delmotte, Valerie, Lohmann, Gerrit
Format: Dataset
Language:English
Published: PANGAEA 2018
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.893855
https://doi.org/10.1594/PANGAEA.893855
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spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.893855 2023-05-15T14:04:57+02:00 ECHAM5-wiso simulation data for Antarctica Werner, Martin Jouzel, Jean Masson-Delmotte, Valerie Lohmann, Gerrit LATITUDE: -90.000000 * LONGITUDE: 0.000000 2018-09-10 text/tab-separated-values, 50 data points https://doi.pangaea.de/10.1594/PANGAEA.893855 https://doi.org/10.1594/PANGAEA.893855 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.893855 https://doi.org/10.1594/PANGAEA.893855 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Werner, Martin; Jouzel, Jean; Masson-Delmotte, Valerie; Lohmann, Gerrit (2018): Reconciling glacial Antarctic water stable isotopes with ice sheet topography and the isotopic paleothermometer. Nature Communications, 9(1), https://doi.org/10.1038/s41467-018-05430-y Antarctica File content File format File name File size Uniform resource locator/link to file Dataset 2018 ftpangaea https://doi.org/10.1594/PANGAEA.893855 https://doi.org/10.1038/s41467-018-05430-y 2023-01-20T09:11:28Z Stable water isotope records from Antarctica are key for our understanding of Quaternary climate variations. However, the exact quantitative interpretation of these important climate proxy records in terms of surface temperature, ice sheet height and other climatic changes is still a matter of debate. Here we report results obtained with an atmospheric general circulation model equipped with water isotopes, run at a high-spatial horizontal resolution of one-by-one degree. Comparing different glacial maximum ice sheet reconstructions, a best model data match is achieved for the PMIP3 reconstruction. Reduced West Antarctic elevation changes between 400 and 800 m lead to further improved agreement with ice core data. Our modern and glacial climate simulations support the validity of the isotopic paleothermometer approach based on the use of present-day observations and reveal that a glacial ocean state as displayed in the GLAMAP reconstruction is suitable for capturing the observed glacial isotope changes in Antarctic ice cores. Dataset Antarc* Antarctic Antarctica ice core Ice Sheet PANGAEA - Data Publisher for Earth & Environmental Science Antarctic ENVELOPE(0.000000,0.000000,-90.000000,-90.000000)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Antarctica
File content
File format
File name
File size
Uniform resource locator/link to file
spellingShingle Antarctica
File content
File format
File name
File size
Uniform resource locator/link to file
Werner, Martin
Jouzel, Jean
Masson-Delmotte, Valerie
Lohmann, Gerrit
ECHAM5-wiso simulation data for Antarctica
topic_facet Antarctica
File content
File format
File name
File size
Uniform resource locator/link to file
description Stable water isotope records from Antarctica are key for our understanding of Quaternary climate variations. However, the exact quantitative interpretation of these important climate proxy records in terms of surface temperature, ice sheet height and other climatic changes is still a matter of debate. Here we report results obtained with an atmospheric general circulation model equipped with water isotopes, run at a high-spatial horizontal resolution of one-by-one degree. Comparing different glacial maximum ice sheet reconstructions, a best model data match is achieved for the PMIP3 reconstruction. Reduced West Antarctic elevation changes between 400 and 800 m lead to further improved agreement with ice core data. Our modern and glacial climate simulations support the validity of the isotopic paleothermometer approach based on the use of present-day observations and reveal that a glacial ocean state as displayed in the GLAMAP reconstruction is suitable for capturing the observed glacial isotope changes in Antarctic ice cores.
format Dataset
author Werner, Martin
Jouzel, Jean
Masson-Delmotte, Valerie
Lohmann, Gerrit
author_facet Werner, Martin
Jouzel, Jean
Masson-Delmotte, Valerie
Lohmann, Gerrit
author_sort Werner, Martin
title ECHAM5-wiso simulation data for Antarctica
title_short ECHAM5-wiso simulation data for Antarctica
title_full ECHAM5-wiso simulation data for Antarctica
title_fullStr ECHAM5-wiso simulation data for Antarctica
title_full_unstemmed ECHAM5-wiso simulation data for Antarctica
title_sort echam5-wiso simulation data for antarctica
publisher PANGAEA
publishDate 2018
url https://doi.pangaea.de/10.1594/PANGAEA.893855
https://doi.org/10.1594/PANGAEA.893855
op_coverage LATITUDE: -90.000000 * LONGITUDE: 0.000000
long_lat ENVELOPE(0.000000,0.000000,-90.000000,-90.000000)
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Antarctica
ice core
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
ice core
Ice Sheet
op_source Supplement to: Werner, Martin; Jouzel, Jean; Masson-Delmotte, Valerie; Lohmann, Gerrit (2018): Reconciling glacial Antarctic water stable isotopes with ice sheet topography and the isotopic paleothermometer. Nature Communications, 9(1), https://doi.org/10.1038/s41467-018-05430-y
op_relation https://doi.pangaea.de/10.1594/PANGAEA.893855
https://doi.org/10.1594/PANGAEA.893855
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.893855
https://doi.org/10.1038/s41467-018-05430-y
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