Present and LGM permafrost from climate simulations: contribution of statistical downscaling

We quantify the agreement between permafrost distributions from PMIP2 (Paleoclimate Modeling Intercomparison Project) climate models and permafrost data. We evaluate the ability of several climate models to represent permafrost and assess the inter-variability between them. Studying an heterogeneous...

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Main Authors: Levavasseur, G., Vrac, M., Roche, Didier M., Paillard, D., Martin, A., Vandenberghe, J.
Other Authors: Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Modélisation du climat (CLIM)
Format: Report
Language:English
Published: HAL CCSD 2021
Subjects:
Gam
Online Access:https://hal.science/hal-03206147
https://hal.science/hal-03206147/document
https://hal.science/hal-03206147/file/tcd-4-2233-2010.pdf
https://doi.org/10.5194/tcd-4-2233-2010
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institution Open Polar
collection Archives ouvertes de Paris-Saclay
op_collection_id ftuniparissaclay
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
Levavasseur, G.
Vrac, M.
Roche, Didier M.
Paillard, D.
Martin, A.
Vandenberghe, J.
Present and LGM permafrost from climate simulations: contribution of statistical downscaling
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
description We quantify the agreement between permafrost distributions from PMIP2 (Paleoclimate Modeling Intercomparison Project) climate models and permafrost data. We evaluate the ability of several climate models to represent permafrost and assess the inter-variability between them. Studying an heterogeneous variable such as permafrost implies to conduct analysis at a smaller spatial scale compared with climate models resolution. Our approach consists in applying statistical downscaling methods (SDMs) on large- or regional-scale atmospheric variables provided by climate models, leading to local permafrost modelling. Among the SDMs, we first choose a transfer function approach based on Generalized Additive Models (GAMs) to produce high-resolution climatology of surface air temperature (SAT). Then, we define permafrost distribution over Eurasia by SAT conditions. In a first validation step on present climate (CTRL period), GAM shows some limitations with non-systemic improvements in comparison with the large-scale fields. So, we develop an alternative method of statistical downscaling based on a stochastic generator approach through a Multinomial Logistic Regression (MLR), which directly models the probabilities of local permafrost indices. The obtained permafrost distributions appear in a better agreement with data. In both cases, the provided local information reduces the inter-variability between climate models. Nevertheless, this also proves that a simple relationship between permafrost and the SAT only is not always sufficient to represent local permafrost. Finally, we apply each method on a very different climate, the Last Glacial Maximum (LGM) time period, in order to quantify the ability of climate models to represent LGM permafrost. Our SDMs do not significantly improve permafrost distribution and do not reduce the inter-variability between climate models, at this period. We show that LGM permafrost distribution from climate models strongly depends on large-scale SAT. The differences with LGM data, larger than in ...
author2 Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)
Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR)
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Modélisation du climat (CLIM)
format Report
author Levavasseur, G.
Vrac, M.
Roche, Didier M.
Paillard, D.
Martin, A.
Vandenberghe, J.
author_facet Levavasseur, G.
Vrac, M.
Roche, Didier M.
Paillard, D.
Martin, A.
Vandenberghe, J.
author_sort Levavasseur, G.
title Present and LGM permafrost from climate simulations: contribution of statistical downscaling
title_short Present and LGM permafrost from climate simulations: contribution of statistical downscaling
title_full Present and LGM permafrost from climate simulations: contribution of statistical downscaling
title_fullStr Present and LGM permafrost from climate simulations: contribution of statistical downscaling
title_full_unstemmed Present and LGM permafrost from climate simulations: contribution of statistical downscaling
title_sort present and lgm permafrost from climate simulations: contribution of statistical downscaling
publisher HAL CCSD
publishDate 2021
url https://hal.science/hal-03206147
https://hal.science/hal-03206147/document
https://hal.science/hal-03206147/file/tcd-4-2233-2010.pdf
https://doi.org/10.5194/tcd-4-2233-2010
long_lat ENVELOPE(-57.955,-57.955,-61.923,-61.923)
geographic Gam
geographic_facet Gam
genre permafrost
genre_facet permafrost
op_source https://hal.science/hal-03206147
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op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/tcd-4-2233-2010
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https://hal.science/hal-03206147
https://hal.science/hal-03206147/document
https://hal.science/hal-03206147/file/tcd-4-2233-2010.pdf
doi:10.5194/tcd-4-2233-2010
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.5194/tcd-4-2233-2010
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spelling ftuniparissaclay:oai:HAL:hal-03206147v1 2024-06-16T07:42:35+00:00 Present and LGM permafrost from climate simulations: contribution of statistical downscaling Levavasseur, G. Vrac, M. Roche, Didier M. Paillard, D. Martin, A. Vandenberghe, J. Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Modélisation du climat (CLIM) 2021-09-16 https://hal.science/hal-03206147 https://hal.science/hal-03206147/document https://hal.science/hal-03206147/file/tcd-4-2233-2010.pdf https://doi.org/10.5194/tcd-4-2233-2010 en eng HAL CCSD info:eu-repo/semantics/altIdentifier/doi/10.5194/tcd-4-2233-2010 hal-03206147 https://hal.science/hal-03206147 https://hal.science/hal-03206147/document https://hal.science/hal-03206147/file/tcd-4-2233-2010.pdf doi:10.5194/tcd-4-2233-2010 info:eu-repo/semantics/OpenAccess https://hal.science/hal-03206147 2021 [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/preprint Preprints, Working Papers, . 2021 ftuniparissaclay https://doi.org/10.5194/tcd-4-2233-2010 2024-05-17T00:05:19Z We quantify the agreement between permafrost distributions from PMIP2 (Paleoclimate Modeling Intercomparison Project) climate models and permafrost data. We evaluate the ability of several climate models to represent permafrost and assess the inter-variability between them. Studying an heterogeneous variable such as permafrost implies to conduct analysis at a smaller spatial scale compared with climate models resolution. Our approach consists in applying statistical downscaling methods (SDMs) on large- or regional-scale atmospheric variables provided by climate models, leading to local permafrost modelling. Among the SDMs, we first choose a transfer function approach based on Generalized Additive Models (GAMs) to produce high-resolution climatology of surface air temperature (SAT). Then, we define permafrost distribution over Eurasia by SAT conditions. In a first validation step on present climate (CTRL period), GAM shows some limitations with non-systemic improvements in comparison with the large-scale fields. So, we develop an alternative method of statistical downscaling based on a stochastic generator approach through a Multinomial Logistic Regression (MLR), which directly models the probabilities of local permafrost indices. The obtained permafrost distributions appear in a better agreement with data. In both cases, the provided local information reduces the inter-variability between climate models. Nevertheless, this also proves that a simple relationship between permafrost and the SAT only is not always sufficient to represent local permafrost. Finally, we apply each method on a very different climate, the Last Glacial Maximum (LGM) time period, in order to quantify the ability of climate models to represent LGM permafrost. Our SDMs do not significantly improve permafrost distribution and do not reduce the inter-variability between climate models, at this period. We show that LGM permafrost distribution from climate models strongly depends on large-scale SAT. The differences with LGM data, larger than in ... Report permafrost Archives ouvertes de Paris-Saclay Gam ENVELOPE(-57.955,-57.955,-61.923,-61.923)