Drought effects on soil greenhouse gas fluxes in a boreal and a temperate forest

Changing water regimes (e.g. drought) have unknown long-term consequences on the stability and resilience of soil microorganisms who determine much of the carbon and nitrogen exchange between the biosphere and atmosphere. Shifts in their activity could feedback into ongoing climate change. In this s...

Full description

Bibliographic Details
Main Authors: Gillespie, L. M., Kolari, P., Kulmala, L., Leitner, Sonja, Pihlatie, M., Zechmeister-Boltenstern, S., Díaz-Pinés, E.
Format: Journal Article
Language:Inglés
Published: Springer 2024
Subjects:
Online Access:https://hdl.handle.net/10568/152105
_version_ 1855528258959835136
author Gillespie, L. M.
Kolari, P.
Kulmala, L.
Leitner, Sonja
Pihlatie, M.
Zechmeister-Boltenstern, S.
Díaz-Pinés, E.
author_browse Díaz-Pinés, E.
Gillespie, L. M.
Kolari, P.
Kulmala, L.
Leitner, Sonja
Pihlatie, M.
Zechmeister-Boltenstern, S.
author_facet Gillespie, L. M.
Kolari, P.
Kulmala, L.
Leitner, Sonja
Pihlatie, M.
Zechmeister-Boltenstern, S.
Díaz-Pinés, E.
author_sort Gillespie, L. M.
collection Repository of Agricultural Research Outputs (CGSpace)
description Changing water regimes (e.g. drought) have unknown long-term consequences on the stability and resilience of soil microorganisms who determine much of the carbon and nitrogen exchange between the biosphere and atmosphere. Shifts in their activity could feedback into ongoing climate change. In this study, we explored soil drought effects on soil greenhouse gas (GHG; CO2, CH4, N2O) fluxes over time in two sites: a boreal, coniferous forest in Finland (Hyytiälä) and a temperate, broadleaf forest in Austria (Rosalia). Topsoil moisture and topsoil temperature data were used to identify soil drought events, defined as when soil moisture is below the soil moisture at the permanent wilting point. Data over multiple years from automated GHG flux chambers installed on the forest floor were then analyzed using generalized additive models (GAM) to study whether GHG fluxes differed before and after drought events and whether there was an overall, multiyear temporal trend. Results showed CO2 and N2O emissions to be more affected by drought and long-term trends at Hyytiälä with increased CO2 emission and decreased N2O emissions both following drought and over the entire measurement period. CH4 uptake increased at both sites both during non-drought periods and as an overall, multiyear trend and was predominantly affected by soil moisture dynamics. Multiyear trends also suggest an increase in soil temperature in the boreal forest and a decrease in soil moisture in the temperate forest. These findings underline forests as an important sink for CH4, possibly with an increasing rate in a future climate.
format Journal Article
id CGSpace152105
institution CGIAR Consortium
language Inglés
publishDate 2024
publishDateRange 2024
publishDateSort 2024
publisher Springer
publisherStr Springer
record_format dspace
spelling CGSpace1521052025-12-08T10:11:39Z Drought effects on soil greenhouse gas fluxes in a boreal and a temperate forest Gillespie, L. M. Kolari, P. Kulmala, L. Leitner, Sonja Pihlatie, M. Zechmeister-Boltenstern, S. Díaz-Pinés, E. climate change climate models resilience water data forests soil drought nitrogen emission temperature measurement trends soil moisture emissions dynamics stability microorganisms soil temperature soil microorganisms greenhouse gas greenhouse moisture Changing water regimes (e.g. drought) have unknown long-term consequences on the stability and resilience of soil microorganisms who determine much of the carbon and nitrogen exchange between the biosphere and atmosphere. Shifts in their activity could feedback into ongoing climate change. In this study, we explored soil drought effects on soil greenhouse gas (GHG; CO2, CH4, N2O) fluxes over time in two sites: a boreal, coniferous forest in Finland (Hyytiälä) and a temperate, broadleaf forest in Austria (Rosalia). Topsoil moisture and topsoil temperature data were used to identify soil drought events, defined as when soil moisture is below the soil moisture at the permanent wilting point. Data over multiple years from automated GHG flux chambers installed on the forest floor were then analyzed using generalized additive models (GAM) to study whether GHG fluxes differed before and after drought events and whether there was an overall, multiyear temporal trend. Results showed CO2 and N2O emissions to be more affected by drought and long-term trends at Hyytiälä with increased CO2 emission and decreased N2O emissions both following drought and over the entire measurement period. CH4 uptake increased at both sites both during non-drought periods and as an overall, multiyear trend and was predominantly affected by soil moisture dynamics. Multiyear trends also suggest an increase in soil temperature in the boreal forest and a decrease in soil moisture in the temperate forest. These findings underline forests as an important sink for CH4, possibly with an increasing rate in a future climate. 2024-03-06 2024-09-11T09:26:00Z 2024-09-11T09:26:00Z Journal Article https://hdl.handle.net/10568/152105 en Open Access Springer Gillespie, L. M., Kolari, P., Kulmala, L., Leitner, S. M., Pihlatie, M., Zechmeister-Boltenstern, S., & Díaz-Pinés, E. (2024). Drought effects on soil greenhouse gas fluxes in a boreal and a temperate forest. Biogeochemistry, 167(2), 155–175. https://doi.org/10.1007/s10533-024-01126-2
spellingShingle climate change
climate
models
resilience
water
data
forests
soil
drought
nitrogen
emission
temperature
measurement
trends
soil moisture
emissions
dynamics
stability
microorganisms
soil temperature
soil microorganisms
greenhouse gas
greenhouse
moisture
Gillespie, L. M.
Kolari, P.
Kulmala, L.
Leitner, Sonja
Pihlatie, M.
Zechmeister-Boltenstern, S.
Díaz-Pinés, E.
Drought effects on soil greenhouse gas fluxes in a boreal and a temperate forest
title Drought effects on soil greenhouse gas fluxes in a boreal and a temperate forest
title_full Drought effects on soil greenhouse gas fluxes in a boreal and a temperate forest
title_fullStr Drought effects on soil greenhouse gas fluxes in a boreal and a temperate forest
title_full_unstemmed Drought effects on soil greenhouse gas fluxes in a boreal and a temperate forest
title_short Drought effects on soil greenhouse gas fluxes in a boreal and a temperate forest
title_sort drought effects on soil greenhouse gas fluxes in a boreal and a temperate forest
topic climate change
climate
models
resilience
water
data
forests
soil
drought
nitrogen
emission
temperature
measurement
trends
soil moisture
emissions
dynamics
stability
microorganisms
soil temperature
soil microorganisms
greenhouse gas
greenhouse
moisture
url https://hdl.handle.net/10568/152105
work_keys_str_mv AT gillespielm droughteffectsonsoilgreenhousegasfluxesinaborealandatemperateforest
AT kolarip droughteffectsonsoilgreenhousegasfluxesinaborealandatemperateforest
AT kulmalal droughteffectsonsoilgreenhousegasfluxesinaborealandatemperateforest
AT leitnersonja droughteffectsonsoilgreenhousegasfluxesinaborealandatemperateforest
AT pihlatiem droughteffectsonsoilgreenhousegasfluxesinaborealandatemperateforest
AT zechmeisterboltensterns droughteffectsonsoilgreenhousegasfluxesinaborealandatemperateforest
AT diazpinese droughteffectsonsoilgreenhousegasfluxesinaborealandatemperateforest