Examining anomalous summer carbonyl sulfide emissions in a boreal forest after thinning

Abstract Carbonyl sulfide (COS) is gaining interest as a proxy for gross primary productivity (GPP). Thinning of the Hyytiälä (Finland) forest in the winter of 2019–2020 altered the response of COS fluxes to environmental conditions in the summer of 2021. For the first time, extended periods of ecosystem-scale COS emissions were observed in a boreal forest. The warm and dry conditions in the summer of 2021 reduced the COS uptake by the canopy and elevated soil abiotic COS production. However, the reduction in canopy uptake and the increase in soil production do not fully explain the observed ecosystem-level emissions. The analysis suggests an unidentified, homogeneously distributed COS source in the eddy covariance footprint area, potentially from the photodegradation of forest floor litter and cutting residue from thinning. Such a source in a boreal forest stand warrants further source apportionment studies to effectively use COS as a proxy for GPP.

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Publication Details

Journal
npj Climate and Atmospheric Science
Published
2026-01-02
DOI
https://doi.org/10.1038/s41612-025-01272-w
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
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article

Examining anomalous summer carbonyl sulfide emissions in a boreal forest after thinning

Ivan Mammarella, Timo Vesala, Roderick C. Dewar, Kukka‐Maaria Kohonen et al.
npj Climate and Atmospheric Science
Atmospheric chemistry and aerosols
article

Examining anomalous summer carbonyl sulfide emissions in a boreal forest after thinning

Ivan Mammarella, Timo Vesala, Roderick C. Dewar, Kukka‐Maaria Kohonen, Yann Salmon, Pasi Kolari, Paulina Dukat, Toprak Aslan, Abin Thomas, Asta Laasonen, Wu Sun, Kadmiel Maseyk
article en

Abstract

Abstract Carbonyl sulfide (COS) is gaining interest as a proxy for gross primary productivity (GPP). Thinning of the Hyytiälä (Finland) forest in the winter of 2019–2020 altered the response of COS fluxes to environmental conditions in the summer of 2021. For the first time, extended periods of ecosystem-scale COS emissions were observed in a boreal forest. The warm and dry conditions in the summer of 2021 reduced the COS uptake by the canopy and elevated soil abiotic COS production. However, the reduction in canopy uptake and the increase in soil production do not fully explain the observed ecosystem-level emissions. The analysis suggests an unidentified, homogeneously distributed COS source in the eddy covariance footprint area, potentially from the photodegradation of forest floor litter and cutting residue from thinning. Such a source in a boreal forest stand warrants further source apportionment studies to effectively use COS as a proxy for GPP.

npj Climate and Atmospheric ScienceVol. 9(1)
Openalex Percentile: Top 99%
Atmospheric chemistry and aerosols
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