Soil thawing regulates the spring growth onset in tundra and alpine biomes
International audience Soil temperature remains isothermal at 0 °C and water shifts to a liquid phase during soil thawing. Vegetation may receive this process as a signal and a key to restore physiological activity. We aimed to show the relationship between the timing of soil thawing and the spring...
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Online Access: | https://hal.archives-ouvertes.fr/hal-03032256 https://hal.archives-ouvertes.fr/hal-03032256/document https://hal.archives-ouvertes.fr/hal-03032256/file/ste.pdf https://doi.org/10.1016/j.scitotenv.2020.140637 |
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ftunivnantes:oai:HAL:hal-03032256v1 2023-05-15T18:40:05+02:00 Soil thawing regulates the spring growth onset in tundra and alpine biomes Descals, Adrià Verger, Aleixandre Filella, Iolanda Baldocchi, Dennis Janssens, Ivan, Fu, Yongshuo, Piao, Shilong Peaucelle, Marc Ciais, Philippe Peñuelas, Josep ICOS-ATC (ICOS-ATC) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) H2020 Marie Skłodowska-Curie Actions, MSCA: 891369 European Research Council, ERC: ERC-SyG-2013-610028 IMBALANCE-P SGR 2017-1005 Fonds Wetenschappelijk Onderzoek, FWO: G018319N PID2019-110521GB-I00 The authors would like to acknowledge the financial support from the European Research Council Synergy grant ERC-SyG-2013-610028 IMBALANCE-P, the Spanish Government grant PID2019-110521GB-I00 and the Catalan Government grant SGR 2017-1005 . M.P. acknowledges the financial support from the Fonds Wetenschappelijk Onderzoek (FWO; grant no. G018319N ) and the H2020 Marie Skłodowska-Curie Actions (LEAF-2-TBM grant no. 891369 ). 2020 https://hal.archives-ouvertes.fr/hal-03032256 https://hal.archives-ouvertes.fr/hal-03032256/document https://hal.archives-ouvertes.fr/hal-03032256/file/ste.pdf https://doi.org/10.1016/j.scitotenv.2020.140637 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.scitotenv.2020.140637 info:eu-repo/semantics/altIdentifier/pmid/32721746 hal-03032256 https://hal.archives-ouvertes.fr/hal-03032256 https://hal.archives-ouvertes.fr/hal-03032256/document https://hal.archives-ouvertes.fr/hal-03032256/file/ste.pdf doi:10.1016/j.scitotenv.2020.140637 PUBMED: 32721746 info:eu-repo/semantics/OpenAccess ISSN: 0048-9697 EISSN: 1879-1026 Science of the Total Environment https://hal.archives-ouvertes.fr/hal-03032256 Science of the Total Environment, Elsevier, 2020, 742, ⟨10.1016/j.scitotenv.2020.140637⟩ Boreal forests Deciduous forests Plant phenology Spring onset Thawing Tundra [SDE]Environmental Sciences info:eu-repo/semantics/article Journal articles 2020 ftunivnantes https://doi.org/10.1016/j.scitotenv.2020.140637 2022-10-18T23:29:41Z International audience Soil temperature remains isothermal at 0 °C and water shifts to a liquid phase during soil thawing. Vegetation may receive this process as a signal and a key to restore physiological activity. We aimed to show the relationship between the timing of soil thawing and the spring growth onset. We estimated the delay between the soil thawing and the spring growth onset in 78 sites of the FLUXNET network. We built a soil thawing map derived from modeling for the northern hemisphere and related it to the greenness onset estimated with satellite imagery. Spring onset estimated with GPP time series occurred shortly after soil surface thawing in tundra (1.1 ± 3.5 days) and alpine grasslands (16.6 ± 5.8 days). The association was weaker for deciduous forests (40.3 ± 4.2 days), especially where soils freeze infrequently. Needleleaved forests tended to start the growing season before the end of thawing (−17.4 ± 3.6 days), although observations from remote sensing (MODIS Land Cover Dynamics) indicated that the onset of greenness started after the thawing period (26.8 ± 3.2 days). This study highlights the role of soil temperature at the spring growth onset at high latitudes. Soil thawing becomes less relevant in temperate forests, where soil is occasionally frozen and other climate factors become more important. Article in Journal/Newspaper Tundra Université de Nantes: HAL-UNIV-NANTES Science of The Total Environment 742 140637 |
institution |
Open Polar |
collection |
Université de Nantes: HAL-UNIV-NANTES |
op_collection_id |
ftunivnantes |
language |
English |
topic |
Boreal forests Deciduous forests Plant phenology Spring onset Thawing Tundra [SDE]Environmental Sciences |
spellingShingle |
Boreal forests Deciduous forests Plant phenology Spring onset Thawing Tundra [SDE]Environmental Sciences Descals, Adrià Verger, Aleixandre Filella, Iolanda Baldocchi, Dennis Janssens, Ivan, Fu, Yongshuo, Piao, Shilong Peaucelle, Marc Ciais, Philippe Peñuelas, Josep Soil thawing regulates the spring growth onset in tundra and alpine biomes |
topic_facet |
Boreal forests Deciduous forests Plant phenology Spring onset Thawing Tundra [SDE]Environmental Sciences |
description |
International audience Soil temperature remains isothermal at 0 °C and water shifts to a liquid phase during soil thawing. Vegetation may receive this process as a signal and a key to restore physiological activity. We aimed to show the relationship between the timing of soil thawing and the spring growth onset. We estimated the delay between the soil thawing and the spring growth onset in 78 sites of the FLUXNET network. We built a soil thawing map derived from modeling for the northern hemisphere and related it to the greenness onset estimated with satellite imagery. Spring onset estimated with GPP time series occurred shortly after soil surface thawing in tundra (1.1 ± 3.5 days) and alpine grasslands (16.6 ± 5.8 days). The association was weaker for deciduous forests (40.3 ± 4.2 days), especially where soils freeze infrequently. Needleleaved forests tended to start the growing season before the end of thawing (−17.4 ± 3.6 days), although observations from remote sensing (MODIS Land Cover Dynamics) indicated that the onset of greenness started after the thawing period (26.8 ± 3.2 days). This study highlights the role of soil temperature at the spring growth onset at high latitudes. Soil thawing becomes less relevant in temperate forests, where soil is occasionally frozen and other climate factors become more important. |
author2 |
ICOS-ATC (ICOS-ATC) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) H2020 Marie Skłodowska-Curie Actions, MSCA: 891369 European Research Council, ERC: ERC-SyG-2013-610028 IMBALANCE-P SGR 2017-1005 Fonds Wetenschappelijk Onderzoek, FWO: G018319N PID2019-110521GB-I00 The authors would like to acknowledge the financial support from the European Research Council Synergy grant ERC-SyG-2013-610028 IMBALANCE-P, the Spanish Government grant PID2019-110521GB-I00 and the Catalan Government grant SGR 2017-1005 . M.P. acknowledges the financial support from the Fonds Wetenschappelijk Onderzoek (FWO; grant no. G018319N ) and the H2020 Marie Skłodowska-Curie Actions (LEAF-2-TBM grant no. 891369 ). |
format |
Article in Journal/Newspaper |
author |
Descals, Adrià Verger, Aleixandre Filella, Iolanda Baldocchi, Dennis Janssens, Ivan, Fu, Yongshuo, Piao, Shilong Peaucelle, Marc Ciais, Philippe Peñuelas, Josep |
author_facet |
Descals, Adrià Verger, Aleixandre Filella, Iolanda Baldocchi, Dennis Janssens, Ivan, Fu, Yongshuo, Piao, Shilong Peaucelle, Marc Ciais, Philippe Peñuelas, Josep |
author_sort |
Descals, Adrià |
title |
Soil thawing regulates the spring growth onset in tundra and alpine biomes |
title_short |
Soil thawing regulates the spring growth onset in tundra and alpine biomes |
title_full |
Soil thawing regulates the spring growth onset in tundra and alpine biomes |
title_fullStr |
Soil thawing regulates the spring growth onset in tundra and alpine biomes |
title_full_unstemmed |
Soil thawing regulates the spring growth onset in tundra and alpine biomes |
title_sort |
soil thawing regulates the spring growth onset in tundra and alpine biomes |
publisher |
HAL CCSD |
publishDate |
2020 |
url |
https://hal.archives-ouvertes.fr/hal-03032256 https://hal.archives-ouvertes.fr/hal-03032256/document https://hal.archives-ouvertes.fr/hal-03032256/file/ste.pdf https://doi.org/10.1016/j.scitotenv.2020.140637 |
genre |
Tundra |
genre_facet |
Tundra |
op_source |
ISSN: 0048-9697 EISSN: 1879-1026 Science of the Total Environment https://hal.archives-ouvertes.fr/hal-03032256 Science of the Total Environment, Elsevier, 2020, 742, ⟨10.1016/j.scitotenv.2020.140637⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.scitotenv.2020.140637 info:eu-repo/semantics/altIdentifier/pmid/32721746 hal-03032256 https://hal.archives-ouvertes.fr/hal-03032256 https://hal.archives-ouvertes.fr/hal-03032256/document https://hal.archives-ouvertes.fr/hal-03032256/file/ste.pdf doi:10.1016/j.scitotenv.2020.140637 PUBMED: 32721746 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1016/j.scitotenv.2020.140637 |
container_title |
Science of The Total Environment |
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742 |
container_start_page |
140637 |
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1766229245896425472 |