Dissolved organic matter properties in arctic coastal waters are strongly influenced by fluxes from permafrost coasts and by local meteorology.

Under future climate change scenarios, Arctic coastal waters are believed to receive higher terrestrial organic matter (OM) fluxes. Permafrost carbon is increasingly mobilized upon thaw from rivers draining permafrost terrain and from eroding permafrost coasts. Once received, the coastal waters are...

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Bibliographic Details
Main Authors: Fritz, Michael, Tanski, George, Goncalves-Araujo, Rafael, Heim, Birgit, Koch, Boris, Lantuit, Hugues
Format: Conference Object
Language:unknown
Published: 2016
Subjects:
Ice
Online Access:https://epic.awi.de/id/eprint/41122/
https://epic.awi.de/id/eprint/41122/1/Abstract_ICOP2016_MFritz.pdf
https://hdl.handle.net/10013/epic.48132
https://hdl.handle.net/10013/epic.48132.d001