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Footprint of temperature changes in the temperate and boreal forest carbon balance

Authors :
Peylin, Philippe
Piao, Shilong
Friedlingstein, P.
Ciais, Philippe
Zhu, B.
Reichstein, M.
College of Urban and Environmental Sciences [Beijing]
Peking University [Beijing]
Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
School of Earth Sciences [Bristol]
University of Bristol [Bristol]
ICOS-ATC (ICOS-ATC)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-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)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Modélisation des Surfaces et Interfaces Continentales (MOSAIC)
University of California
Max Planck Institute for Biogeochemistry (MPI-BGC)
Max-Planck-Gesellschaft
Biogéochimie et écologie des milieux continentaux (Bioemco)
Centre National de la Recherche Scientifique (CNRS)-AgroParisTech-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut National de la Recherche Agronomique (INRA)-École normale supérieure - Paris (ENS Paris)
Université Paris-Saclay-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)
Laboratoire Dynamique de la Biodiversité (LADYBIO)
Université Toulouse III - Paul Sabatier (UT3)
Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-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)
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)
University of California (UC)
Source :
Geophysical Research Letters, Geophysical Research Letters, American Geophysical Union, 2009, 36, pp.L07404. ⟨10.1029/2009GL037381⟩, Geophysical Research Letters, American Geophysical Union, 2009, L07404 (5 pp.), Geophysical Research Letters, 2009, 36, pp.L07404. ⟨10.1029/2009GL037381⟩
Publication Year :
2009

Abstract

International audience; In this study, we use net ecosystem productivity (NEP) measurement data across several forest sites and a simple conceptual model to investigate the linkage between temperature and NEP by considering either temperature change in the recent past or current mean annual temperature (MAT) as a forcing. After removing the effect of stand age, forest NEP is only weakly correlated with MAT. However, temperature changes during the period of 1980-2002 do explain a very significant fraction of the current spatial patterns of NEP, although the response of the terrestrial carbon balance to temperature changes varies with season. Changes in spring temperature having the highest correlation with annual NEP. We also show that temperature changes before the 1970s had a limited influence on the current NEP, and that the impact of recent temperature changes within the last decade on NEP are not strong enough to be observable. Overall, our analysis indicates not only that temperature changes in the recent past is one of the important drivers of today's forest carbon balance in the Northern Hemisphere, but also that the ongoing global warming will contribute significantly to the near-future evolution of the Northern Hemisphere carbon sink. A non-equilibrium framework must be taken into account when studying the impacts of temperature change on current or future forest net carbon balance.

Subjects

Subjects :
[SDE]Environmental Sciences

Details

ISSN :
00948276 and 19448007
Database :
OpenAIRE
Journal :
Geophysical Research Letters, Geophysical Research Letters, American Geophysical Union, 2009, 36, pp.L07404. ⟨10.1029/2009GL037381⟩, Geophysical Research Letters, American Geophysical Union, 2009, L07404 (5 pp.), Geophysical Research Letters, 2009, 36, pp.L07404. ⟨10.1029/2009GL037381⟩
Accession number :
edsair.dedup.wf.001..200b1111beeafcfd2764b303b3d35eb4