Summer drought weakens land surface cooling of tundra vegetation

Siberia experienced a prolonged heatwave in the spring of 2020, resulting in extreme summer drought and major wildfires in the North-Eastern Siberian lowland tundra. In the Arctic tundra, plants play a key role in regulating the summer land surface energy budget by contributing to land surface cooli...

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Main Authors: Nils Rietze, Jakob J Assmann, Elena Plekhanova, Kathrin Naegeli, Alexander Damm, Trofim C Maximov, Sergey V Karsanaev, Geert Hensgens, Gabriela Schaepman-Strub
Format: Article
Language:English
Published: IOP Publishing 2024-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/ad345e
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author Nils Rietze
Jakob J Assmann
Elena Plekhanova
Kathrin Naegeli
Alexander Damm
Trofim C Maximov
Sergey V Karsanaev
Geert Hensgens
Gabriela Schaepman-Strub
author_facet Nils Rietze
Jakob J Assmann
Elena Plekhanova
Kathrin Naegeli
Alexander Damm
Trofim C Maximov
Sergey V Karsanaev
Geert Hensgens
Gabriela Schaepman-Strub
author_sort Nils Rietze
collection DOAJ
description Siberia experienced a prolonged heatwave in the spring of 2020, resulting in extreme summer drought and major wildfires in the North-Eastern Siberian lowland tundra. In the Arctic tundra, plants play a key role in regulating the summer land surface energy budget by contributing to land surface cooling through evapotranspiration. Yet we know little about how drought conditions impact land surface cooling by tundra plant communities, potentially contributing to high air temperatures through a positive plant-mediated feedback. Here we used high-resolution land surface temperature and vegetation maps based on drone imagery to determine the impact of an extreme summer drought on land surface cooling in the lowland tundra of North-Eastern Siberia. We found that land surface cooling differed strongly among plant communities between the drought year 2020 and the reference year 2021. Further, we observed a decrease in the normalized land surface cooling (measured as water deficit index) in the drought year 2020 across all plant communities. This indicates a shift towards an energy budget dominated by sensible heat fluxes, contributing to land surface warming. Overall, our findings suggest significant variation in land surface cooling among common Arctic plant communities in the North-Eastern Siberian lowland tundra and a pronounced effect of drought on all community types. Based on our results, we suggest discriminating between functional tundra plant communities when predicting the drought impacts on energy flux related processes such as land surface cooling, permafrost thaw and wildfires.
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spelling doaj.art-a67d4446badc4c79879b787581a12da42024-03-22T09:46:23ZengIOP PublishingEnvironmental Research Letters1748-93262024-01-0119404404310.1088/1748-9326/ad345eSummer drought weakens land surface cooling of tundra vegetationNils Rietze0https://orcid.org/0000-0001-7232-7799Jakob J Assmann1https://orcid.org/0000-0002-3492-8419Elena Plekhanova2https://orcid.org/0000-0002-5727-9175Kathrin Naegeli3https://orcid.org/0000-0003-2443-7154Alexander Damm4https://orcid.org/0000-0001-8965-3427Trofim C Maximov5Sergey V Karsanaev6https://orcid.org/0000-0002-4055-381XGeert Hensgens7https://orcid.org/0000-0001-6511-7224Gabriela Schaepman-Strub8https://orcid.org/0000-0002-4069-1884Department of Evolutionary Biology and Environmental Studies, University of Zurich , Zurich, Switzerland; Department of Geography, University of Zurich , Zurich, SwitzerlandDepartment of Evolutionary Biology and Environmental Studies, University of Zurich , Zurich, SwitzerlandDepartment of Evolutionary Biology and Environmental Studies, University of Zurich , Zurich, SwitzerlandDepartment of Geography, University of Zurich , Zurich, SwitzerlandDepartment of Geography, University of Zurich , Zurich, Switzerland; Eawag, Swiss Federal Institute of Aquatic Science and Technology , 8600 Dübendorf, SwitzerlandInstitute for Biological Problems of the Cryolithozone, Siberian Branch Russian Academy of Sciences , Yakutsk, RussiaInstitute for Biological Problems of the Cryolithozone, Siberian Branch Russian Academy of Sciences , Yakutsk, RussiaDepartment of Earth and Climate, Vrije Universiteit Amsterdam , Amsterdam, The NetherlandsDepartment of Evolutionary Biology and Environmental Studies, University of Zurich , Zurich, SwitzerlandSiberia experienced a prolonged heatwave in the spring of 2020, resulting in extreme summer drought and major wildfires in the North-Eastern Siberian lowland tundra. In the Arctic tundra, plants play a key role in regulating the summer land surface energy budget by contributing to land surface cooling through evapotranspiration. Yet we know little about how drought conditions impact land surface cooling by tundra plant communities, potentially contributing to high air temperatures through a positive plant-mediated feedback. Here we used high-resolution land surface temperature and vegetation maps based on drone imagery to determine the impact of an extreme summer drought on land surface cooling in the lowland tundra of North-Eastern Siberia. We found that land surface cooling differed strongly among plant communities between the drought year 2020 and the reference year 2021. Further, we observed a decrease in the normalized land surface cooling (measured as water deficit index) in the drought year 2020 across all plant communities. This indicates a shift towards an energy budget dominated by sensible heat fluxes, contributing to land surface warming. Overall, our findings suggest significant variation in land surface cooling among common Arctic plant communities in the North-Eastern Siberian lowland tundra and a pronounced effect of drought on all community types. Based on our results, we suggest discriminating between functional tundra plant communities when predicting the drought impacts on energy flux related processes such as land surface cooling, permafrost thaw and wildfires.https://doi.org/10.1088/1748-9326/ad345eArctictundradroughtSiberialand surface temperaturedrones
spellingShingle Nils Rietze
Jakob J Assmann
Elena Plekhanova
Kathrin Naegeli
Alexander Damm
Trofim C Maximov
Sergey V Karsanaev
Geert Hensgens
Gabriela Schaepman-Strub
Summer drought weakens land surface cooling of tundra vegetation
Environmental Research Letters
Arctic
tundra
drought
Siberia
land surface temperature
drones
title Summer drought weakens land surface cooling of tundra vegetation
title_full Summer drought weakens land surface cooling of tundra vegetation
title_fullStr Summer drought weakens land surface cooling of tundra vegetation
title_full_unstemmed Summer drought weakens land surface cooling of tundra vegetation
title_short Summer drought weakens land surface cooling of tundra vegetation
title_sort summer drought weakens land surface cooling of tundra vegetation
topic Arctic
tundra
drought
Siberia
land surface temperature
drones
url https://doi.org/10.1088/1748-9326/ad345e
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AT alexanderdamm summerdroughtweakenslandsurfacecoolingoftundravegetation
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