The permafrost thaw fingerprint: the Isotopic composition of Particulate Organic Carbon From Lena River to Laptev sea

Rapid climate warming in the Arctic region intensifies permafrost thaw, increases active layer depth in summer and enhances riverbank and coastal erosion. This causes the release of organic matter (OM) into streams and rivers and result in discharge of terrestrial OM into the Arctic Ocean. The focus...

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Bibliographic Details
Main Authors: Ogneva, Olga, Mollenhauer, Gesine, Grotheer, Hendrik, Fuchs, Matthias, Palmtag, Juri, Mann, Paul James, Strauss, Jens
Format: Conference Object
Language:unknown
Published: 2021
Subjects:
Online Access:https://epic.awi.de/id/eprint/53923/
https://hdl.handle.net/10013/epic.51b081e9-611a-49e9-a9a0-88247535369d