Articles | Volume 9, issue 2
The Cryosphere, 9, 737–752, 2015
https://doi.org/10.5194/tc-9-737-2015
The Cryosphere, 9, 737–752, 2015
https://doi.org/10.5194/tc-9-737-2015

Research article 20 Apr 2015

Research article | 20 Apr 2015

Dissolved organic carbon (DOC) in Arctic ground ice

M. Fritz et al.

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Michael Fritz on behalf of the Authors (15 Mar 2015)  Author's response    Manuscript
ED: Publish subject to minor revisions (Editor review) (24 Mar 2015) by Stephan Gruber
AR by Michael Fritz on behalf of the Authors (26 Mar 2015)  Author's response    Manuscript
ED: Publish subject to technical corrections (26 Mar 2015) by Stephan Gruber
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Short summary
Ground ice in permafrost has not, until now, been considered to be a source of dissolved organic carbon (DOC), dissolved inorganic carbon (DIC) and other elements that are important for ecosystems and carbon cycling. Ice wedges in the Arctic Yedoma region hold 45.2 Tg DOC (Tg = 10^12g), 33.6 Tg DIC and a freshwater reservoir of 4200 km³. Leaching of terrestrial organic matter is the most relevant process of DOC sequestration into ground ice.