Temperature extremes of 2022 reduced carbon uptake by forests in Europe

Auke M. van der Woude*, Wouter Peters, Emilie Joetzjer, Sébastien Lafont, Gerbrand Koren, Philippe Ciais, Michel Ramonet, Yidi Xu, Ana Bastos, Santiago Botía, Stephen Sitch, Remco de Kok, Tobias Kneuer, Dagmar Kubistin, Adrien Jacotot, Benjamin Loubet, Pedro-Henrique Herig-Coimbra, Denis Loustau, Ingrid T. Luijkx

*Corresponding author for this work

Research output: Contribution to journalArticleAcademicpeer-review

Abstract

The year 2022 saw record breaking temperatures in Europe during both summer and fall. Similar to the recent 2018 drought, close to 30% (3.0 million km2) of the European continent was under severe summer drought. In 2022, the drought was located in central and southeastern Europe, contrasting the Northern-centered 2018 drought. We show, using multiple sets of observations, a reduction of net biospheric carbon uptake in summer (56-62 TgC) over the drought area. Specific sites in France even showed a widespread summertime carbon release by forests, additional to wildfires. Partial compensation (32%) for the decreased carbon uptake due to drought was offered by a warm autumn with prolonged biospheric carbon uptake. The severity of this second drought event in 5 years suggests drought-induced reduced carbon uptake to no longer be exceptional, and important to factor into Europe’s developing plans for net-zero greenhouse gas emissions that rely on carbon uptake by forests.
Original languageEnglish
Article number6218
Number of pages11
JournalNature Communications
Volume14
Issue number1
DOIs
Publication statusPublished - Dec 2023

Bibliographical note

Publisher Copyright:
© 2023, Springer Nature Limited.

Funding

We acknowledge NWO/ENW (file number 2023.003) and SURF for supercomputing facilities. We furthermore acknowledge the PARIS project funded by the European Union under the Grant Agreement nr 101081430, NWO (Vidi grant VI.Vidi.213.143) and the Ruisdael Observatory, which is (partly) financed by the Dutch Research Council (NWO, grant number 184.034.015) for financial support. Furthermore, we thank the ICOS Carbon Portal for hosting the CTE-HR fluxes. We kindly acknowledge the provision of data from eddy-covariance sites80, as well as from atmospheric sites86. The measurements at WAO are funded by the UK’s National Centre for Atmospheric Sciences (NCAS). CO2 observations at Jungfraujoch are supported by ICOS Switzerland (ICOS-CH) Phase 3 (Swiss National Science Foundation, grant 20F120_198227). CH-Dav was supported by the SNF projects ICOS-CH Phase 1-3 (20FI21_148992, 143 20FI20_173691, 20F120_198227) and the EU project RINGO 730944. We acknowledge Guido van der Werf for his help on the fire flux estimates and kindly thank Imme Benedict for providing the GPH data. We also thank Thomas Koch and Saqr Munassar for pre-processing the meteorological data for the atmospheric transport with STILT. We acknowledge NWO/ENW (file number 2023.003) and SURF for supercomputing facilities. We furthermore acknowledge the PARIS project funded by the European Union under the Grant Agreement nr 101081430, NWO (Vidi grant VI.Vidi.213.143) and the Ruisdael Observatory, which is (partly) financed by the Dutch Research Council (NWO, grant number 184.034.015) for financial support. Furthermore, we thank the ICOS Carbon Portal for hosting the CTE-HR fluxes. We kindly acknowledge the provision of data from eddy-covariance sites, as well as from atmospheric sites. The measurements at WAO are funded by the UK’s National Centre for Atmospheric Sciences (NCAS). CO observations at Jungfraujoch are supported by ICOS Switzerland (ICOS-CH) Phase 3 (Swiss National Science Foundation, grant 20F120_198227). CH-Dav was supported by the SNF projects ICOS-CH Phase 1-3 (20FI21_148992, 143 20FI20_173691, 20F120_198227) and the EU project RINGO 730944. We acknowledge Guido van der Werf for his help on the fire flux estimates and kindly thank Imme Benedict for providing the GPH data. We also thank Thomas Koch and Saqr Munassar for pre-processing the meteorological data for the atmospheric transport with STILT. 2

FundersFunder number
ENW2023.003
ICOS-CH
STILT
SURF
National Centre for Atmospheric Science
European Commission730944, 101081430
Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung20FI21_148992, 20F120_198227, 143 20FI20_173691
Nederlandse Organisatie voor Wetenschappelijk OnderzoekVI.Vidi.213.143, 184.034.015
Integrated Carbon Observation System

    Keywords

    • Assimilation
    • Co2
    • Drought events
    • Fluxes
    • Heat
    • Impacts
    • Net ecosystem exchange
    • Respiration
    • Separation
    • Summer

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