Earlier snowmelt may lead to late season declines in plant productivity and carbon sequestration in Arctic tundra ecosystems

International audience Arctic warming is affecting snow cover and soil hydrology, with consequences for carbon sequestration in tundra ecosystems. The scarcity of observations in the Arctic has limited our understanding of the impact of covarying environmental drivers on the carbon balance of tundra...

Full description

Bibliographic Details
Published in:Scientific Reports
Main Authors: Zona, Donatella, Lafleur, Peter, Hufkens, Koen, Bailey, Barbara, Gioli, Beniamino, Burba, George, Goodrich, Jordan, Liljedahl, Anna, Euskirchen, Eugénie, Watts, Jennifer, Farina, Mary, Kimball, John, Heimann, Martin, Göckede, Mathias, Pallandt, Martijn, Christensen, Torben, Mastepanov, Mikhail, López-Blanco, Efrén, Jackowicz-Korczynski, Marcin, Dolman, Albertus, Marchesini, Luca Belelli, Commane, Roisin, Wofsy, Steven, Miller, Charles, Lipson, David, Hashemi, Josh, Arndt, Kyle, Kutzbach, Lars, Holl, David, Boike, Julia, Wille, Christian, Sachs, Torsten, Kalhori, Aram, Song, Xia, Xu, Xiaofeng, Humphreys, Elyn, Koven, Charles, Sonnentag, Oliver, Meyer, Gesa, Gosselin, Gabriel, Marsh, Philip, Oechel, Walter
Other Authors: San Diego State University (SDSU), University of Sheffield Sheffield, Trent University, Universiteit Gent = Ghent University (UGENT), Interactions Sol Plante Atmosphère (UMR ISPA), Ecole Nationale Supérieure des Sciences Agronomiques de Bordeaux-Aquitaine (Bordeaux Sciences Agro)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Institute for BioEconomy Sesto Fiorentino (IBE, National Research Council of Italy, University of Nebraska–Lincoln, University of Nebraska System, University of Waikato Hamilton, University of Alaska Fairbanks (UAF), Institute of Arctic Biology, University of Montana, Woodwell Climate Research Center, Max-Planck-Institut für Biogeochemie (MPI-BGC), Max Planck Institute for Biogeochemistry (MPI-BGC), Max-Planck-Gesellschaft, Aarhus University Aarhus, Vrije Universiteit Amsterdam Amsterdam (VU), Peoples Friendship University of Russia RUDN University (RUDN), Columbia University New York, Harvard University, Jet Propulsion Laboratory (JPL), NASA-California Institute of Technology (CALTECH), University of New Hampshire (UNH), Universität Hamburg (UHH), German Research Centre for Geosciences - Helmholtz-Centre Potsdam (GFZ), Carleton University, Lawrence Berkeley National Laboratory Berkeley (LBNL), Université de Montréal (UdeM), Wilfrid Laurier University (WLU)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2022
Subjects:
Online Access:https://hal.inrae.fr/hal-03642434
https://hal.inrae.fr/hal-03642434/document
https://hal.inrae.fr/hal-03642434/file/2022-Zona-SR.pdf
https://doi.org/10.1038/s41598-022-07561-1
Description
Summary:International audience Arctic warming is affecting snow cover and soil hydrology, with consequences for carbon sequestration in tundra ecosystems. The scarcity of observations in the Arctic has limited our understanding of the impact of covarying environmental drivers on the carbon balance of tundra ecosystems. In this study, we address some of these uncertainties through a novel record of 119 site-years of summer data from eddy covariance towers representing dominant tundra vegetation types located on continuous permafrost in the Arctic. Here we found that earlier snowmelt was associated with more tundra net CO2 sequestration and higher gross primary productivity (GPP) only in June and July, but with lower net carbon sequestration and lower GPP in August. Although higher evapotranspiration (ET) can result in soil drying with the progression of the summer, we did not find significantly lower soil moisture with earlier snowmelt, nor evidence that water stress affected GPP in the late growing season. Our results suggest that the expected increased CO2 sequestration arising from Arctic warming and the associated increase in growing season length may not materialize if tundra ecosystems are not able to continue sequestering CO2 later in the season.