Daugherty Water for Food Global Institute

 

Authors

Donatella Zona, San Diego State University
Peter M. Lafleur, Trent University
Koen Hufkens, BlueGreen Labs
Beniamino Gioli, Consiglio Nazionale delle Ricerche
Barbara Bailey, San Diego State University
George Burba, LI COR Biosciences
Eugénie S. Euskirchen, University of Alaska Fairbanks
Jennifer D. Watts, Woodwell Climate Research Center
Kyle A. Arndt, Woodwell Climate Research Center
Mary Farina, Woodwell Climate Research Center
John S. Kimball, University of Montana
Martin Heimann, Max Planck Institute for Biogeochemistry
Mathias Göckede, Max Planck Institute for Biogeochemistry
Martijn Pallandt, Max Planck Institute for Biogeochemistry
Torben R. Christensen, Aarhus Universitet
Mikhail Mastepanov, Aarhus Universitet
Efrén López-Blanco, Aarhus Universitet
Albertus J. Dolman, Royal Netherlands Institute for Sea Research - NIOZ
Roisin Commane, Lamont-Doherty Earth Observatory
Charles E. Miller, California Institute of Technology
Josh Hashemi, San Diego State University
Lars Kutzbach, Universität Hamburg
David Holl, Universität Hamburg
Julia Boike, Humboldt-Universität zu Berlin
Christian Wille, Deutsches GeoForschungsZentrum (GFZ)
Torsten Sachs, Deutsches GeoForschungsZentrum (GFZ)
Aram Kalhori, Deutsches GeoForschungsZentrum (GFZ)
Elyn R. Humphreys, Carleton University
Oliver Sonnentag, University of Montreal
Gesa Meyer, University of Montreal
Gabriel H. Gosselin, University of Montreal
Philip Marsh, Wilfrid Laurier University
Walter C. Oechel, San Diego State University

Date of this Version

3-1-2023

Document Type

Article

Citation

Glob Change Biol. 2022;00:1–15.

DOI: 10.1111/gcb.16487

Comments

This is an open access article under the terms of the Creative Commons Attribution License,

Abstract

Long-term atmospheric CO2 concentration records have suggested a reduction in the positive effect of warming on high-latitude carbon uptake since the 1990s. A variety of mechanisms have been proposed to explain the reduced net carbon sink of northern ecosystems with increased air temperature, including water stress on vegetation and increased respiration over recent decades. However, the lack of consistent long-term carbon flux and in situ soil moisture data has severely limited our ability to identify the mechanisms responsible for the recent reduced carbon sink strength. In this study, we used a record of nearly 100 site-years of eddy covariance data from 11 continuous permafrost tundra sites distributed across the circumpolar Arctic to test the temperature (expressed as growing degree days, GDD) responses of gross primary production (GPP), net ecosystem exchange (NEE), and ecosystem respiration (ER) at different periods of the summer (early, peak, and late summer) including dominant tundra vegetation classes (graminoids and mosses, and shrubs). We further tested GPP, NEE, and ER relationships with soil moisture and vapor pressure deficit to identify potential moisture limitations on plant productivity and net carbon exchange. Our results show a decrease in GPP with rising GDD during the peak summer (July) for both vegetation classes, and a significant relationship between the peak summer GPP and soil moisture after statistically controlling for GDD in a partial correlation analysis. These results suggest that tundra ecosystems might not benefit from increased temperature as much as suggested by several terrestrial biosphere models, if decreased soil moisture limits the peak summer plant productivity, reducing the ability of these ecosystems to sequester carbon during the summer.

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