Thaw pond expansion enhances greenhouse gas emissions in the Northeast Siberian tundra.

Thaw of surficial permafrost ice bodies (ice wedges and ice-rich mounds) causes formation of ponds with enhanced emission of CH4 and CO2 . Usually these ponds develop in dry Betula nana shrub vegetation, which, when undisturbed, is a sink for both greenhouse gases. We mapped thaw pond development ov...

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Bibliographic Details
Main Authors: van Huissteden, J., Heijmans, MMPD, Dean, J.F., Teshebaeva, K.
Format: Conference Object
Language:English
Published: 2018
Subjects:
Ice
Online Access:https://research.vu.nl/en/publications/4777743a-158b-427f-b3ee-28d45dd9ca65
http://hdl.handle.net/1871.1/4777743a-158b-427f-b3ee-28d45dd9ca65