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...

Full description

Bibliographic Details
Published in:The Cryosphere
Main Authors: Parazoo, Nicholas C., Koven, Charles D., Lawrence, David M., Romanovsky, Vladimir, Miller, Charles E.
Format: Text
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.5194/tc-12-123-2018
https://tc.copernicus.org/articles/12/123/2018/