Summer warming explains widespread but not uniform greening in the Arctic tundra biome

Author:

Berner Logan T.ORCID,Massey RichardORCID,Jantz PatrickORCID,Forbes Bruce C.ORCID,Macias-Fauria MarcORCID,Myers-Smith IslaORCID,Kumpula Timo,Gauthier GillesORCID,Andreu-Hayles LaiaORCID,Gaglioti Benjamin V.,Burns PatrickORCID,Zetterberg Pentti,D’Arrigo Rosanne,Goetz Scott J.ORCID

Abstract

AbstractArctic warming can influence tundra ecosystem function with consequences for climate feedbacks, wildlife and human communities. Yet ecological change across the Arctic tundra biome remains poorly quantified due to field measurement limitations and reliance on coarse-resolution satellite data. Here, we assess decadal changes in Arctic tundra greenness using time series from the 30 m resolution Landsat satellites. From 1985 to 2016 tundra greenness increased (greening) at ~37.3% of sampling sites and decreased (browning) at ~4.7% of sampling sites. Greening occurred most often at warm sampling sites with increased summer air temperature, soil temperature, and soil moisture, while browning occurred most often at cold sampling sites that cooled and dried. Tundra greenness was positively correlated with graminoid, shrub, and ecosystem productivity measured at field sites. Our results support the hypothesis that summer warming stimulated plant productivity across much, but not all, of the Arctic tundra biome during recent decades.

Funder

National Aeronautics and Space Administration

Academy of Finland

Joint Program Initiative Climate

United Kingdom National Environmental Research Council

ArcticNet

Environment and Climate Change Canada

Natural Science and Engineering Research Council of Canada Polar Continental Shelf Program

National Science Foundation

Lamont-Doherty Earth Observatory Climate Center

Joint Fire Science Program

Publisher

Springer Science and Business Media LLC

Subject

General Physics and Astronomy,General Biochemistry, Genetics and Molecular Biology,General Chemistry

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