Evaluation of current and projected Antarctic precipitation in CMIP5 models

International audience On average, the models in the Fifth Climate Model Intercomparison Project archive predict an increase in Antarctic precipitation from 5.5 to 24.5 % between 1986-2005 and 2080-2099, depending on greenhouse gas emissions scenarios. This translates into a moderation of future sea...

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Published in:Climate Dynamics
Main Authors: Palerme, Cyril, Genthon, Christophe, Claud, Chantal, Kay, Jennifer E., Wood, Norman B., L'Ecuyer, Tristan
Other Authors: Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X), Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-École nationale des ponts et chaussées (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS-PSL, École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL), ANR-15-CE01-0003,APRES3,Les précipitations antarctiques : télédétection depuis la surface et l'espace(2015)
Format: Article in Journal/Newspaper
Language:English
Published: CCSD 2017
Subjects:
Online Access:https://insu.hal.science/insu-03727090
https://insu.hal.science/insu-03727090v1/document
https://insu.hal.science/insu-03727090v1/file/Palerme2017_Article_EvaluationOfCurrentAndProjecte.pdf
https://doi.org/10.1007/s00382-016-3071-1
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author Palerme, Cyril
Genthon, Christophe
Claud, Chantal
Kay, Jennifer E.
Wood, Norman B.
L'Ecuyer, Tristan
author2 Laboratoire de Météorologie Dynamique (UMR 8539) (LMD)
Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)
Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-École nationale des ponts et chaussées (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS-PSL
École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)
ANR-15-CE01-0003,APRES3,Les précipitations antarctiques : télédétection depuis la surface et l'espace(2015)
author_facet Palerme, Cyril
Genthon, Christophe
Claud, Chantal
Kay, Jennifer E.
Wood, Norman B.
L'Ecuyer, Tristan
author_sort Palerme, Cyril
collection Archives ouvertes de Paris-Saclay
container_issue 1-2
container_start_page 225
container_title Climate Dynamics
container_volume 48
description International audience On average, the models in the Fifth Climate Model Intercomparison Project archive predict an increase in Antarctic precipitation from 5.5 to 24.5 % between 1986-2005 and 2080-2099, depending on greenhouse gas emissions scenarios. This translates into a moderation of future sea level rise ranging from -19 to -71 mm between 2006 and 2099. However, comparison with CloudSat and ERA-Interim data show that almost all the models overestimate current Antarctic precipitation, some by more than 100 %. If only the models that agree with CloudSat data within 20 % of error are considered, larger precipitation changes (from 7.4 to 29.3 %) and impact on sea level (from -25 to -85 mm) are predicted. A common practice of averaging all models to evaluate climate projections thus leads to a significant underestimation of the contribution of Antarctic precipitation to future sea level. Models simulate, on average, a 7.4 %/°C precipitation change with surface temperature warming. The models in better agreement with CloudSat observations for Antarctic snowfall predict, on average, larger temperature and Antarctic sea ice cover changes, which could explain the larger changes in Antarctic precipitation simulated by these models. The agreement between the models, CloudSat data and ERA-Interim is generally less in the interior of Antarctica than at the peripheries, but the interior is also where climate change will induce the smallest absolute change in precipitation. About three-quarters of the impact on sea level will result from precipitation change over the half most peripheral and lowest elevation part of the surface of Antarctica.
format Article in Journal/Newspaper
genre Antarc*
Antarctic
Antarctica
Sea ice
genre_facet Antarc*
Antarctic
Antarctica
Sea ice
geographic Antarctic
geographic_facet Antarctic
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op_doi https://doi.org/10.1007/s00382-016-3071-1
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-016-3071-1
BIBCODE: 2017ClDy.48.225P
op_rights http://creativecommons.org/licenses/by/
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op_source ISSN: 0930-7575
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Climate Dynamics
https://insu.hal.science/insu-03727090
Climate Dynamics, 2017, 48, pp.225-239. ⟨10.1007/s00382-016-3071-1⟩
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spelling ftuniparissaclay:oai:HAL:insu-03727090v1 2025-02-23T14:44:03+00:00 Evaluation of current and projected Antarctic precipitation in CMIP5 models Palerme, Cyril Genthon, Christophe Claud, Chantal Kay, Jennifer E. Wood, Norman B. L'Ecuyer, Tristan Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-École nationale des ponts et chaussées (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS-PSL École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL) ANR-15-CE01-0003,APRES3,Les précipitations antarctiques : télédétection depuis la surface et l'espace(2015) 2017 https://insu.hal.science/insu-03727090 https://insu.hal.science/insu-03727090v1/document https://insu.hal.science/insu-03727090v1/file/Palerme2017_Article_EvaluationOfCurrentAndProjecte.pdf https://doi.org/10.1007/s00382-016-3071-1 en eng CCSD Springer Verlag info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-016-3071-1 BIBCODE: 2017ClDy.48.225P http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 0930-7575 EISSN: 1432-0894 Climate Dynamics https://insu.hal.science/insu-03727090 Climate Dynamics, 2017, 48, pp.225-239. ⟨10.1007/s00382-016-3071-1⟩ Antarctica Precipitation CloudSat CMIP5 Sea level [SDU]Sciences of the Universe [physics] [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2017 ftuniparissaclay https://doi.org/10.1007/s00382-016-3071-1 2025-01-24T02:00:35Z International audience On average, the models in the Fifth Climate Model Intercomparison Project archive predict an increase in Antarctic precipitation from 5.5 to 24.5 % between 1986-2005 and 2080-2099, depending on greenhouse gas emissions scenarios. This translates into a moderation of future sea level rise ranging from -19 to -71 mm between 2006 and 2099. However, comparison with CloudSat and ERA-Interim data show that almost all the models overestimate current Antarctic precipitation, some by more than 100 %. If only the models that agree with CloudSat data within 20 % of error are considered, larger precipitation changes (from 7.4 to 29.3 %) and impact on sea level (from -25 to -85 mm) are predicted. A common practice of averaging all models to evaluate climate projections thus leads to a significant underestimation of the contribution of Antarctic precipitation to future sea level. Models simulate, on average, a 7.4 %/°C precipitation change with surface temperature warming. The models in better agreement with CloudSat observations for Antarctic snowfall predict, on average, larger temperature and Antarctic sea ice cover changes, which could explain the larger changes in Antarctic precipitation simulated by these models. The agreement between the models, CloudSat data and ERA-Interim is generally less in the interior of Antarctica than at the peripheries, but the interior is also where climate change will induce the smallest absolute change in precipitation. About three-quarters of the impact on sea level will result from precipitation change over the half most peripheral and lowest elevation part of the surface of Antarctica. Article in Journal/Newspaper Antarc* Antarctic Antarctica Sea ice Archives ouvertes de Paris-Saclay Antarctic Climate Dynamics 48 1-2 225 239
spellingShingle Antarctica
Precipitation
CloudSat
CMIP5
Sea level
[SDU]Sciences of the Universe [physics]
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
Palerme, Cyril
Genthon, Christophe
Claud, Chantal
Kay, Jennifer E.
Wood, Norman B.
L'Ecuyer, Tristan
Evaluation of current and projected Antarctic precipitation in CMIP5 models
title Evaluation of current and projected Antarctic precipitation in CMIP5 models
title_full Evaluation of current and projected Antarctic precipitation in CMIP5 models
title_fullStr Evaluation of current and projected Antarctic precipitation in CMIP5 models
title_full_unstemmed Evaluation of current and projected Antarctic precipitation in CMIP5 models
title_short Evaluation of current and projected Antarctic precipitation in CMIP5 models
title_sort evaluation of current and projected antarctic precipitation in cmip5 models
topic Antarctica
Precipitation
CloudSat
CMIP5
Sea level
[SDU]Sciences of the Universe [physics]
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
topic_facet Antarctica
Precipitation
CloudSat
CMIP5
Sea level
[SDU]Sciences of the Universe [physics]
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
url https://insu.hal.science/insu-03727090
https://insu.hal.science/insu-03727090v1/document
https://insu.hal.science/insu-03727090v1/file/Palerme2017_Article_EvaluationOfCurrentAndProjecte.pdf
https://doi.org/10.1007/s00382-016-3071-1