Articles | Volume 20, issue 11
https://doi.org/10.5194/bg-20-2031-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-20-2031-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Snow–vegetation–atmosphere interactions in alpine tundra
Department of Geosciences, University of Oslo, Oslo, Norway
Kristoffer Aalstad
Department of Geosciences, University of Oslo, Oslo, Norway
Yeliz A. Yilmaz
Department of Geosciences, University of Oslo, Oslo, Norway
Astrid Vatne
Department of Geosciences, University of Oslo, Oslo, Norway
Andrea L. Popp
Department of Geosciences, University of Oslo, Oslo, Norway
Hydrological Research Unit, Swedish Meteorological and Hydrological Institute (SMHI), Norrköping, Sweden
Peter Horvath
Natural History Museum, University of Oslo, Oslo, Norway
Anders Bryn
Natural History Museum, University of Oslo, Oslo, Norway
Ane Victoria Vollsnes
Department of Biosciences, University of Oslo, Oslo, Norway
Sebastian Westermann
Department of Geosciences, University of Oslo, Oslo, Norway
Terje Koren Berntsen
Department of Geosciences, University of Oslo, Oslo, Norway
Frode Stordal
Department of Geosciences, University of Oslo, Oslo, Norway
Lena Merete Tallaksen
Department of Geosciences, University of Oslo, Oslo, Norway
Data sets
Resources for "Snow-vegetation-atmosphere interactions in alpine tundra" Norbert Pirk, Kristoffer Aalstad, Yeliz A. Yilmaz, Astrid Vatne, Andrea L. Popp, Peter Horvath, Anders Bryn, Ane Victoria Vollsnes, Sebastian Westermann, Terje Koren Berntsen, Frode Stordal, and Lena Merete Tallaksen https://doi.org/10.5281/zenodo.7566641
geco-nhm/NiN\_Finse: Finse\_publication (finse) Peter Horvath https://doi.org/10.5281/zenodo.8005237
Short summary
We measured the land–atmosphere exchange of CO2 and water vapor in alpine Norway over 3 years. The extremely snow-rich conditions in 2020 reduced the total annual evapotranspiration to 50 % and reduced the growing-season carbon assimilation to turn the ecosystem from a moderate annual carbon sink to an even stronger source. Our analysis suggests that snow cover anomalies are driving the most consequential short-term responses in this ecosystem’s functioning.
We measured the land–atmosphere exchange of CO2 and water vapor in alpine Norway over 3 years....
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