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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ftuniparissaclay:oai:HAL:insu-03727090v1 2024-09-15T17:47:14+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 des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris 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) 2017 https://insu.hal.science/insu-03727090 https://insu.hal.science/insu-03727090/document https://insu.hal.science/insu-03727090/file/Palerme2017_Article_EvaluationOfCurrentAndProjecte.pdf https://doi.org/10.1007/s00382-016-3071-1 en eng HAL CCSD Springer Verlag info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-016-3071-1 insu-03727090 https://insu.hal.science/insu-03727090 https://insu.hal.science/insu-03727090/document https://insu.hal.science/insu-03727090/file/Palerme2017_Article_EvaluationOfCurrentAndProjecte.pdf BIBCODE: 2017ClDy.48.225P doi:10.1007/s00382-016-3071-1 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 2024-08-30T01:48:53Z 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 Climate Dynamics 48 1-2 225 239 |
institution |
Open Polar |
collection |
Archives ouvertes de Paris-Saclay |
op_collection_id |
ftuniparissaclay |
language |
English |
topic |
Antarctica Precipitation CloudSat CMIP5 Sea level [SDU]Sciences of the Universe [physics] [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
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 |
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 |
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. |
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 des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris 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) |
format |
Article in Journal/Newspaper |
author |
Palerme, Cyril Genthon, Christophe Claud, Chantal Kay, Jennifer E. Wood, Norman B. L'Ecuyer, Tristan |
author_facet |
Palerme, Cyril Genthon, Christophe Claud, Chantal Kay, Jennifer E. Wood, Norman B. L'Ecuyer, Tristan |
author_sort |
Palerme, Cyril |
title |
Evaluation of current and projected Antarctic precipitation in CMIP5 models |
title_short |
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_sort |
evaluation of current and projected antarctic precipitation in cmip5 models |
publisher |
HAL CCSD |
publishDate |
2017 |
url |
https://insu.hal.science/insu-03727090 https://insu.hal.science/insu-03727090/document https://insu.hal.science/insu-03727090/file/Palerme2017_Article_EvaluationOfCurrentAndProjecte.pdf https://doi.org/10.1007/s00382-016-3071-1 |
genre |
Antarc* Antarctic Antarctica Sea ice |
genre_facet |
Antarc* Antarctic Antarctica Sea ice |
op_source |
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⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-016-3071-1 insu-03727090 https://insu.hal.science/insu-03727090 https://insu.hal.science/insu-03727090/document https://insu.hal.science/insu-03727090/file/Palerme2017_Article_EvaluationOfCurrentAndProjecte.pdf BIBCODE: 2017ClDy.48.225P doi:10.1007/s00382-016-3071-1 |
op_rights |
http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1007/s00382-016-3071-1 |
container_title |
Climate Dynamics |
container_volume |
48 |
container_issue |
1-2 |
container_start_page |
225 |
op_container_end_page |
239 |
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1810496148132069376 |