Detecting the permafrost carbon feedback: Talik formation and increased cold-season respiration as precursors to sink-to-source transitions

Thaw and release of permafrost carbon (C) due to climate change is likely to offset increased vegetation C uptake in northern high-latitude (NHL) terrestrial ecosystems. Models project that this permafrost C feedback may act as a slow leak, in which case detection and attribution of the feedback may...

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Bibliographic Details
Main Authors: Parazoo, NC, Koven, CD, Lawrence, DM, Romanovsky, V, Miller, CE
Format: Article in Journal/Newspaper
Language:unknown
Published: eScholarship, University of California 2018
Subjects:
Online Access:https://escholarship.org/uc/item/5z6634d2