CO2-induced terrestrial climate feedback mechanism : From carbon sink to aerosol source and back

Feedbacks mechanisms are essential components of our climate system, as they either increase or decrease changes in climate-related quantities in the presence of external forcings. In this work, we provide the first quantitative estimate regarding the terrestrial climate feedback loop connecting the increasing atmospheric carbon dioxide concentration, changes in gross primary production (GPP) associated with the carbon uptake, organic aerosol formation in the atmosphere, and transfer of both diffuse and global radiation. Our approach was to combine process-level understanding with comprehensive, long-term field measurement data set collected from a boreal forest site in southern Finland. Our best estimate of the gain in GPP resulting from the feedback is 1.3 (range 1.02-1.5), which is larger than the gains of the few atmospheric chemistry-climate feedbacks estimated using large-scale models. Our analysis demonstrates the power of using comprehensive field measurements in investigating the complicated couplings between the biosphere and atmosphere on one hand, and the need for complementary approaches relying on the combination of field data, satellite observations model simulations on the other hand.

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Publication Details

Journal
Työväentutkimus Vuosikirja
Published
2024-12-12
DOI
https://doi.org/10.60910/e3ex-cwgh
Citations
88
Primary Topic
Atmospheric and Environmental Gas Dynamics
Type
article
Field-Weighted Citation Impact
3.39

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article

CO2-induced terrestrial climate feedback mechanism : From carbon sink to aerosol source and back

Markku Kulmala, Erik Swietlicki, Jaana Bäck, Timo Vesala et al.
88 citations
Työväentutkimus Vuosikirja
Atmospheric and Environmental Gas Dynamics
3.39
article

CO2-induced terrestrial climate feedback mechanism : From carbon sink to aerosol source and back

Markku Kulmala, Erik Swietlicki, Jaana Bäck, Timo Vesala, M. K. Kajos, Hans‐Christen Hansson, Tuomo Nieminen, Katrianne Lehtipalo, Antti Lauri, Hanna E. Manninen, Radovan Krejčí, Torben R. Christensen, Pasi Kolari, Almut Arneth, Tuukka Petäjä, Veli‐Matti Kerminen, Anders Lindroth, Anna Nikandrova, Pertti Hari
article en
88 citations

Abstract

Feedbacks mechanisms are essential components of our climate system, as they either increase or decrease changes in climate-related quantities in the presence of external forcings. In this work, we provide the first quantitative estimate regarding the terrestrial climate feedback loop connecting the increasing atmospheric carbon dioxide concentration, changes in gross primary production (GPP) associated with the carbon uptake, organic aerosol formation in the atmosphere, and transfer of both diffuse and global radiation. Our approach was to combine process-level understanding with comprehensive, long-term field measurement data set collected from a boreal forest site in southern Finland. Our best estimate of the gain in GPP resulting from the feedback is 1.3 (range 1.02-1.5), which is larger than the gains of the few atmospheric chemistry-climate feedbacks estimated using large-scale models. Our analysis demonstrates the power of using comprehensive field measurements in investigating the complicated couplings between the biosphere and atmosphere on one hand, and the need for complementary approaches relying on the combination of field data, satellite observations model simulations on the other hand.

Työväentutkimus VuosikirjaVol. 19
Stockholm University (SE), Institute of Nuclear Physics (UZ)
Strong
Climate action
Openalex Percentile: Top 8%
Atmospheric and Environmental Gas Dynamics
3.39
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