Permafrost thaw driven changes in hydrology and vegetation cover increase trace gas emissions and climate forcing in Stordalen Mire from 1970 to 2014
Permafrost thaw increases active layer thickness, changes landscape hydrology and influences vegetation species composition. These changes alter belowground microbial and geochemical processes, affecting production, consumption and net emission rates of climate forcing trace gases. Net carbon dioxid...
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Published in | Philosophical transactions of the Royal Society of London. Series A: Mathematical, physical, and engineering sciences Vol. 380; no. 2215; p. 20210022 |
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Main Authors | , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
England
The Royal Society Publishing
24.01.2022
The Royal Society |
Subjects | |
Online Access | Get full text |
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