Land–atmosphere interactions in sub-polar and alpine climates in the CORDEX Flagship Pilot Study Land Use and Climate Across Scales (LUCAS) models – Part 2: The role of changing vegetation

International audience Abstract. Land cover in sub-polar and alpine regions of northern and eastern Europe have already begun changing due to natural and anthropogenic changes such as afforestation. This will impact the regional climate and hydrology upon which societies in these regions are highly...

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Published in:The Cryosphere
Main Authors: Mooney, Priscilla, Rechid, Diana, Davin, Edouard, Katragkou, Eleni, de Noblet-Ducoudré, Natalie, Breil, Marcus, Cardoso, Rita, Daloz, Anne Sophie, Hoffmann, Peter, Lima, Daniela, Meier, Ronny, Soares, Pedro, Sofiadis, Giannis, Strada, Susanna, Strandberg, Gustav, Toelle, Merja, Lund, Marianne, Daloz, Anne
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))
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2022
Subjects:
Online Access:https://hal.science/hal-03657399
https://hal.science/hal-03657399/document
https://hal.science/hal-03657399/file/tc-16-1383-2022.pdf
https://doi.org/10.5194/tc-16-1383-2022
id ftceafr:oai:HAL:hal-03657399v1
record_format openpolar
institution Open Polar
collection HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives)
op_collection_id ftceafr
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
Mooney, Priscilla
Rechid, Diana
Davin, Edouard
Katragkou, Eleni
de Noblet-Ducoudré, Natalie
Breil, Marcus
Cardoso, Rita
Daloz, Anne Sophie
Hoffmann, Peter
Lima, Daniela
Meier, Ronny
Soares, Pedro
Sofiadis, Giannis
Strada, Susanna
Strandberg, Gustav
Toelle, Merja
Lund, Marianne
Daloz, Anne
Land–atmosphere interactions in sub-polar and alpine climates in the CORDEX Flagship Pilot Study Land Use and Climate Across Scales (LUCAS) models – Part 2: The role of changing vegetation
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
description International audience Abstract. Land cover in sub-polar and alpine regions of northern and eastern Europe have already begun changing due to natural and anthropogenic changes such as afforestation. This will impact the regional climate and hydrology upon which societies in these regions are highly reliant. This study aims to identify the impacts of afforestation/reforestation (hereafter afforestation) on snow and the snow-albedo effect and highlight potential improvements for future model development. The study uses an ensemble of nine regional climate models for two different idealised experiments covering a 30-year period; one experiment replaces most land cover in Europe with forest, while the other experiment replaces all forested areas with grass. The ensemble consists of nine regional climate models composed of different combinations of five regional atmospheric models and six land surface models. Results show that afforestation reduces the snow-albedo sensitivity index and enhances snowmelt. While the direction of change is robustly modelled, there is still uncertainty in the magnitude of change. The greatest differences between models emerge in the snowmelt season. One regional climate model uses different land surface models which shows consistent changes between the three simulations during the accumulation period but differs in the snowmelt season. Together these results point to the need for further model development in representing both grass–snow and forest–snow interactions during the snowmelt season. Pathways to accomplishing this include (1) a more sophisticated representation of forest structure, (2) kilometre-scale simulations, and (3) more observational studies on vegetation–snow interactions in northern Europe.
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))
format Article in Journal/Newspaper
author Mooney, Priscilla
Rechid, Diana
Davin, Edouard
Katragkou, Eleni
de Noblet-Ducoudré, Natalie
Breil, Marcus
Cardoso, Rita
Daloz, Anne Sophie
Hoffmann, Peter
Lima, Daniela
Meier, Ronny
Soares, Pedro
Sofiadis, Giannis
Strada, Susanna
Strandberg, Gustav
Toelle, Merja
Lund, Marianne
Daloz, Anne
author_facet Mooney, Priscilla
Rechid, Diana
Davin, Edouard
Katragkou, Eleni
de Noblet-Ducoudré, Natalie
Breil, Marcus
Cardoso, Rita
Daloz, Anne Sophie
Hoffmann, Peter
Lima, Daniela
Meier, Ronny
Soares, Pedro
Sofiadis, Giannis
Strada, Susanna
Strandberg, Gustav
Toelle, Merja
Lund, Marianne
Daloz, Anne
author_sort Mooney, Priscilla
title Land–atmosphere interactions in sub-polar and alpine climates in the CORDEX Flagship Pilot Study Land Use and Climate Across Scales (LUCAS) models – Part 2: The role of changing vegetation
title_short Land–atmosphere interactions in sub-polar and alpine climates in the CORDEX Flagship Pilot Study Land Use and Climate Across Scales (LUCAS) models – Part 2: The role of changing vegetation
title_full Land–atmosphere interactions in sub-polar and alpine climates in the CORDEX Flagship Pilot Study Land Use and Climate Across Scales (LUCAS) models – Part 2: The role of changing vegetation
title_fullStr Land–atmosphere interactions in sub-polar and alpine climates in the CORDEX Flagship Pilot Study Land Use and Climate Across Scales (LUCAS) models – Part 2: The role of changing vegetation
title_full_unstemmed Land–atmosphere interactions in sub-polar and alpine climates in the CORDEX Flagship Pilot Study Land Use and Climate Across Scales (LUCAS) models – Part 2: The role of changing vegetation
title_sort land–atmosphere interactions in sub-polar and alpine climates in the cordex flagship pilot study land use and climate across scales (lucas) models – part 2: the role of changing vegetation
publisher HAL CCSD
publishDate 2022
url https://hal.science/hal-03657399
https://hal.science/hal-03657399/document
https://hal.science/hal-03657399/file/tc-16-1383-2022.pdf
https://doi.org/10.5194/tc-16-1383-2022
genre The Cryosphere
genre_facet The Cryosphere
op_source ISSN: 1994-0424
EISSN: 1994-0416
The Cryosphere
https://hal.science/hal-03657399
The Cryosphere, 2022, 16 (4), pp.1383 - 1397. ⟨10.5194/tc-16-1383-2022⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-16-1383-2022
hal-03657399
https://hal.science/hal-03657399
https://hal.science/hal-03657399/document
https://hal.science/hal-03657399/file/tc-16-1383-2022.pdf
doi:10.5194/tc-16-1383-2022
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.5194/tc-16-1383-2022
container_title The Cryosphere
container_volume 16
container_issue 4
container_start_page 1383
op_container_end_page 1397
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spelling ftceafr:oai:HAL:hal-03657399v1 2024-09-09T20:11:36+00:00 Land–atmosphere interactions in sub-polar and alpine climates in the CORDEX Flagship Pilot Study Land Use and Climate Across Scales (LUCAS) models – Part 2: The role of changing vegetation Mooney, Priscilla Rechid, Diana Davin, Edouard Katragkou, Eleni de Noblet-Ducoudré, Natalie Breil, Marcus Cardoso, Rita Daloz, Anne Sophie Hoffmann, Peter Lima, Daniela Meier, Ronny Soares, Pedro Sofiadis, Giannis Strada, Susanna Strandberg, Gustav Toelle, Merja Lund, Marianne Daloz, Anne 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)) 2022-04-20 https://hal.science/hal-03657399 https://hal.science/hal-03657399/document https://hal.science/hal-03657399/file/tc-16-1383-2022.pdf https://doi.org/10.5194/tc-16-1383-2022 en eng HAL CCSD Copernicus info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-16-1383-2022 hal-03657399 https://hal.science/hal-03657399 https://hal.science/hal-03657399/document https://hal.science/hal-03657399/file/tc-16-1383-2022.pdf doi:10.5194/tc-16-1383-2022 info:eu-repo/semantics/OpenAccess ISSN: 1994-0424 EISSN: 1994-0416 The Cryosphere https://hal.science/hal-03657399 The Cryosphere, 2022, 16 (4), pp.1383 - 1397. ⟨10.5194/tc-16-1383-2022⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2022 ftceafr https://doi.org/10.5194/tc-16-1383-2022 2024-07-22T13:11:38Z International audience Abstract. Land cover in sub-polar and alpine regions of northern and eastern Europe have already begun changing due to natural and anthropogenic changes such as afforestation. This will impact the regional climate and hydrology upon which societies in these regions are highly reliant. This study aims to identify the impacts of afforestation/reforestation (hereafter afforestation) on snow and the snow-albedo effect and highlight potential improvements for future model development. The study uses an ensemble of nine regional climate models for two different idealised experiments covering a 30-year period; one experiment replaces most land cover in Europe with forest, while the other experiment replaces all forested areas with grass. The ensemble consists of nine regional climate models composed of different combinations of five regional atmospheric models and six land surface models. Results show that afforestation reduces the snow-albedo sensitivity index and enhances snowmelt. While the direction of change is robustly modelled, there is still uncertainty in the magnitude of change. The greatest differences between models emerge in the snowmelt season. One regional climate model uses different land surface models which shows consistent changes between the three simulations during the accumulation period but differs in the snowmelt season. Together these results point to the need for further model development in representing both grass–snow and forest–snow interactions during the snowmelt season. Pathways to accomplishing this include (1) a more sophisticated representation of forest structure, (2) kilometre-scale simulations, and (3) more observational studies on vegetation–snow interactions in northern Europe. Article in Journal/Newspaper The Cryosphere HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives) The Cryosphere 16 4 1383 1397