Polygonal tundra geomorphological change in response to warming alters future CO2 and CH4 flux on the Barrow Peninsula

Global Change Biology

Volumn 21, Issue 4, 2015, Pages 1634-1651

  Lara, Mark J ^a   Mcguire, A David ^a   Euskirchen, Eugenie S ^a   Tweedie, Craig E ^b   Hinkel, Kenneth M ^c   Skurikhin, Alexei N ^d   Romanovsky, Vladimir E ^a,e   Grosse, Guido ^f   Bolton, W Robert ^a   Genet, Helene ^a  

^a UNIVERSITY OF ALASKA FAIRBANKS   (United States)

^b UNIVERSITY OF TEXAS AT EL PASO   (United States)

^c UNIVERSITY OF CINCINNATI   (United States)

^d LOS ALAMOS NATIONAL LABORATORY   (United States)

^e TYUMEN INDUSTRIAL UNIVERSITY   (Russian Federation)

^f ALFRED WEGENER INSTITUTE FOR POLAR AND MARINE RESEARCH   (Germany)

Author keywords

Arctic; Carbon balance; Classification; Climate warming; Negative feedback; Polygonal tundra; Thaw lake cycle; Thermokarst

Indexed keywords

CARBON BALANCE; CARBON FLUX; GEOMORPHOLOGICAL RESPONSE; GLOBAL WARMING; LANDSCAPE CHANGE; METHANE; THERMOKARST; TUNDRA;

ALASKA; ARCTIC; BARROW; UNITED STATES;

CARBON DIOXIDE; METHANE; SOIL;

ALASKA; ARCTIC; CARBON CYCLE; CHEMISTRY; CLIMATE CHANGE; GEOGRAPHIC AND GEOLOGICAL PHENOMENA; SEASON; SOIL; TUNDRA;

ALASKA; ARCTIC REGIONS; CARBON CYCLE; CARBON DIOXIDE; CLIMATE CHANGE; GEOLOGICAL PROCESSES; METHANE; SEASONS; SOIL; TUNDRA;

EID: 84924536643     PISSN: 13541013     EISSN: 13652486     Source Type: Journal    
DOI: 10.1111/gcb.12757     Document Type: Article

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