Multi-year observations reveal a larger than expected autumn respiration signal across northeast Eurasia

International audience Site-level observations have shown pervasive cold season CO 2 release across Arctic and boreal ecosystems, impacting annual carbon budgets. Still, the seasonality of CO 2 emissions are poorly quantified across much of the high latitudes due to the sparse coverage of site-level...

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Published in:Biogeosciences
Main Authors: Byrne, Brendan, Liu, Junjie, Yi, Yonghong, Chatterjee, Abhishek, Basu, Sourish, Cheng, Rui, Doughty, Russell, Chevallier, Frédéric, Bowman, Kevin W., Parazoo, Nicholas C., Crisp, David, Li, Xing, Xiao, Jingfeng, Sitch, Stephen, Guenet, Bertrand, Deng, Feng, Johnson, Matthew S., Philip, Sajeev, Mcguire, Patrick C., Miller, Charles E.
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), Laboratoire de géologie de l'ENS (LGENS), Institut national des sciences de l'Univers (INSU - CNRS)-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), This research has been supported by the National Aeronautics and Space Administration (grant nos. 80NSSC21K1068, NNH17ZDA001N-OCO2, and NNH18ZDA001N-TE).
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2022
Subjects:
CO2
Online Access:https://insu.hal.science/insu-03824351
https://insu.hal.science/insu-03824351/document
https://insu.hal.science/insu-03824351/file/bg-19-4779-2022.pdf
https://doi.org/10.5194/bg-19-4779-2022
id ftinsu:oai:HAL:insu-03824351v1
record_format openpolar
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic CO2
Arctic
Boreal ecosystems
Soil carbon
[SDU]Sciences of the Universe [physics]
spellingShingle CO2
Arctic
Boreal ecosystems
Soil carbon
[SDU]Sciences of the Universe [physics]
Byrne, Brendan
Liu, Junjie
Yi, Yonghong
Chatterjee, Abhishek
Basu, Sourish
Cheng, Rui
Doughty, Russell
Chevallier, Frédéric
Bowman, Kevin W.
Parazoo, Nicholas C.
Crisp, David
Li, Xing
Xiao, Jingfeng
Sitch, Stephen
Guenet, Bertrand
Deng, Feng
Johnson, Matthew S.
Philip, Sajeev
Mcguire, Patrick C.
Miller, Charles E.
Multi-year observations reveal a larger than expected autumn respiration signal across northeast Eurasia
topic_facet CO2
Arctic
Boreal ecosystems
Soil carbon
[SDU]Sciences of the Universe [physics]
description International audience Site-level observations have shown pervasive cold season CO 2 release across Arctic and boreal ecosystems, impacting annual carbon budgets. Still, the seasonality of CO 2 emissions are poorly quantified across much of the high latitudes due to the sparse coverage of site-level observations. Space-based observations provide the opportunity to fill some observational gaps for studying these high-latitude ecosystems, particularly across poorly sampled regions of Eurasia. Here, we show that data-driven net ecosystem exchange (NEE) from atmospheric CO 2 observations implies strong summer uptake followed by strong autumn release of CO 2 over the entire cold northeastern region of Eurasia during the 2015-2019 study period. Combining data-driven NEE with satellite-based estimates of gross primary production (GPP), we show that this seasonality implies less summer heterotrophic respiration (R h ) and greater autumn R h than would be expected given an exponential relationship between respiration and surface temperature. Furthermore, we show that this seasonality of NEE and R h over northeastern Eurasia is not captured by the TRENDY v8 ensemble of dynamic global vegetation models (DGVMs), which estimate that 47 %-57 % (interquartile range) of annual R h occurs during August-April, while the data-driven estimates suggest 59 %-76 % of annual R h occurs over this period. We explain this seasonal shift in R h by respiration from soils at depth during the zero-curtain period, when sub-surface soils remain unfrozen up to several months after the surface has frozen. Additional impacts of physical processes related to freeze-thaw dynamics may contribute to the seasonality of R h . This study confirms a significant and spatially extensive early cold season CO 2 efflux in the permafrost-rich region of northeast Eurasia and suggests that autumn R h from subsurface soils in the northern high latitudes is not well captured by current DGVMs.
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)
Laboratoire de géologie de l'ENS (LGENS)
Institut national des sciences de l'Univers (INSU - CNRS)-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)
This research has been supported by the National Aeronautics and Space Administration (grant nos. 80NSSC21K1068, NNH17ZDA001N-OCO2, and NNH18ZDA001N-TE).
format Article in Journal/Newspaper
author Byrne, Brendan
Liu, Junjie
Yi, Yonghong
Chatterjee, Abhishek
Basu, Sourish
Cheng, Rui
Doughty, Russell
Chevallier, Frédéric
Bowman, Kevin W.
Parazoo, Nicholas C.
Crisp, David
Li, Xing
Xiao, Jingfeng
Sitch, Stephen
Guenet, Bertrand
Deng, Feng
Johnson, Matthew S.
Philip, Sajeev
Mcguire, Patrick C.
Miller, Charles E.
author_facet Byrne, Brendan
Liu, Junjie
Yi, Yonghong
Chatterjee, Abhishek
Basu, Sourish
Cheng, Rui
Doughty, Russell
Chevallier, Frédéric
Bowman, Kevin W.
Parazoo, Nicholas C.
Crisp, David
Li, Xing
Xiao, Jingfeng
Sitch, Stephen
Guenet, Bertrand
Deng, Feng
Johnson, Matthew S.
Philip, Sajeev
Mcguire, Patrick C.
Miller, Charles E.
author_sort Byrne, Brendan
title Multi-year observations reveal a larger than expected autumn respiration signal across northeast Eurasia
title_short Multi-year observations reveal a larger than expected autumn respiration signal across northeast Eurasia
title_full Multi-year observations reveal a larger than expected autumn respiration signal across northeast Eurasia
title_fullStr Multi-year observations reveal a larger than expected autumn respiration signal across northeast Eurasia
title_full_unstemmed Multi-year observations reveal a larger than expected autumn respiration signal across northeast Eurasia
title_sort multi-year observations reveal a larger than expected autumn respiration signal across northeast eurasia
publisher HAL CCSD
publishDate 2022
url https://insu.hal.science/insu-03824351
https://insu.hal.science/insu-03824351/document
https://insu.hal.science/insu-03824351/file/bg-19-4779-2022.pdf
https://doi.org/10.5194/bg-19-4779-2022
genre Arctic
permafrost
genre_facet Arctic
permafrost
op_source ISSN: 1726-4170
EISSN: 1726-4189
Biogeosciences
https://insu.hal.science/insu-03824351
Biogeosciences, 2022, 19, pp.4779-4799. ⟨10.5194/bg-19-4779-2022⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/bg-19-4779-2022
insu-03824351
https://insu.hal.science/insu-03824351
https://insu.hal.science/insu-03824351/document
https://insu.hal.science/insu-03824351/file/bg-19-4779-2022.pdf
BIBCODE: 2022BGeo.19.4779B
doi:10.5194/bg-19-4779-2022
op_rights http://creativecommons.org/licenses/by/
info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.5194/bg-19-4779-2022
container_title Biogeosciences
container_volume 19
container_issue 19
container_start_page 4779
op_container_end_page 4799
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spelling ftinsu:oai:HAL:insu-03824351v1 2024-04-28T08:09:56+00:00 Multi-year observations reveal a larger than expected autumn respiration signal across northeast Eurasia Byrne, Brendan Liu, Junjie Yi, Yonghong Chatterjee, Abhishek Basu, Sourish Cheng, Rui Doughty, Russell Chevallier, Frédéric Bowman, Kevin W. Parazoo, Nicholas C. Crisp, David Li, Xing Xiao, Jingfeng Sitch, Stephen Guenet, Bertrand Deng, Feng Johnson, Matthew S. Philip, Sajeev Mcguire, Patrick C. Miller, Charles E. 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) Laboratoire de géologie de l'ENS (LGENS) Institut national des sciences de l'Univers (INSU - CNRS)-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) This research has been supported by the National Aeronautics and Space Administration (grant nos. 80NSSC21K1068, NNH17ZDA001N-OCO2, and NNH18ZDA001N-TE). 2022 https://insu.hal.science/insu-03824351 https://insu.hal.science/insu-03824351/document https://insu.hal.science/insu-03824351/file/bg-19-4779-2022.pdf https://doi.org/10.5194/bg-19-4779-2022 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/bg-19-4779-2022 insu-03824351 https://insu.hal.science/insu-03824351 https://insu.hal.science/insu-03824351/document https://insu.hal.science/insu-03824351/file/bg-19-4779-2022.pdf BIBCODE: 2022BGeo.19.4779B doi:10.5194/bg-19-4779-2022 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 1726-4170 EISSN: 1726-4189 Biogeosciences https://insu.hal.science/insu-03824351 Biogeosciences, 2022, 19, pp.4779-4799. ⟨10.5194/bg-19-4779-2022⟩ CO2 Arctic Boreal ecosystems Soil carbon [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/article Journal articles 2022 ftinsu https://doi.org/10.5194/bg-19-4779-2022 2024-04-05T00:31:05Z International audience Site-level observations have shown pervasive cold season CO 2 release across Arctic and boreal ecosystems, impacting annual carbon budgets. Still, the seasonality of CO 2 emissions are poorly quantified across much of the high latitudes due to the sparse coverage of site-level observations. Space-based observations provide the opportunity to fill some observational gaps for studying these high-latitude ecosystems, particularly across poorly sampled regions of Eurasia. Here, we show that data-driven net ecosystem exchange (NEE) from atmospheric CO 2 observations implies strong summer uptake followed by strong autumn release of CO 2 over the entire cold northeastern region of Eurasia during the 2015-2019 study period. Combining data-driven NEE with satellite-based estimates of gross primary production (GPP), we show that this seasonality implies less summer heterotrophic respiration (R h ) and greater autumn R h than would be expected given an exponential relationship between respiration and surface temperature. Furthermore, we show that this seasonality of NEE and R h over northeastern Eurasia is not captured by the TRENDY v8 ensemble of dynamic global vegetation models (DGVMs), which estimate that 47 %-57 % (interquartile range) of annual R h occurs during August-April, while the data-driven estimates suggest 59 %-76 % of annual R h occurs over this period. We explain this seasonal shift in R h by respiration from soils at depth during the zero-curtain period, when sub-surface soils remain unfrozen up to several months after the surface has frozen. Additional impacts of physical processes related to freeze-thaw dynamics may contribute to the seasonality of R h . This study confirms a significant and spatially extensive early cold season CO 2 efflux in the permafrost-rich region of northeast Eurasia and suggests that autumn R h from subsurface soils in the northern high latitudes is not well captured by current DGVMs. Article in Journal/Newspaper Arctic permafrost Institut national des sciences de l'Univers: HAL-INSU Biogeosciences 19 19 4779 4799