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The Cryosphere
An interactive open-access journal of the European Geosciences Union
Journal topic
- About
- Editorial board
- Articles
- Special issues
- Highlight articles
- Manuscript tracking
- Subscribe to alerts
- Peer review
- For authors
- For reviewers
- EGU publications
- Imprint
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IF 4.790
5.921CiteScore
5.27SNIP 1.551
SJR 3.016
index 63h5-index 51
Abstracted/indexed
Abstracted/indexed
Volume 9, issue 2
The Cryosphere, 9, 737–752, 2015
https://doi.org/10.5194/tc-9-737-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-9-737-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 9, 737–752, 2015
https://doi.org/10.5194/tc-9-737-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-9-737-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
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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Total article views: 627 (including HTML, PDF, and XML)
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17 citations as recorded by crossref.
- Prokaryotic community in Pleistocene ice wedges of Mammoth Mountain A. Rakitin et al. 10.1007/s00792-019-01138-z
- Sedimentary and geochemical characteristics of two small permafrost-dominated Arctic river deltas in northern Alaska M. Fuchs et al. 10.1007/s41063-018-0056-9
- Eroding permafrost coasts release low amounts of dissolved organic carbon (DOC) from ground ice into the nearshore zone of the Arctic Ocean G. Tanski et al. 10.1002/2015GB005337
- Ice wedges as archives of winter paleoclimate: A review T. Opel et al. 10.1002/ppp.1980
- Holocene ice-wedge polygon development in northern Yukon permafrost peatlands (Canada) M. Fritz et al. 10.1016/j.quascirev.2016.02.008
- Dissolved organic carbon in permafrost regions: A review Q. Ma et al. 10.1007/s11430-018-9309-6
- Reviews and syntheses: Effects of permafrost thaw on Arctic aquatic ecosystems J. Vonk et al. 10.5194/bg-12-7129-2015
- Reviews and Syntheses: Effects of permafrost thaw on arctic aquatic ecosystems J. Vonk et al. 10.5194/bgd-12-10719-2015
- Variability in transport of terrigenous material on the shelves and the deep Arctic Ocean during the Holocene C. Wegner et al. 10.3402/polar.v34.24964
- Deep Yedoma permafrost: A synthesis of depositional characteristics and carbon vulnerability J. Strauss et al. 10.1016/j.earscirev.2017.07.007
- Transformation of terrestrial organic matter along thermokarst-affected permafrost coasts in the Arctic G. Tanski et al. 10.1016/j.scitotenv.2016.12.152
- Retrogressive thaw slumps temper dissolved organic carbon delivery to streams of the Peel Plateau, NWT, Canada C. Littlefair et al. 10.5194/bg-14-5487-2017
- Patterns and rates of riverbank erosion involving ice-rich permafrost (yedoma) in northern Alaska M. Kanevskiy et al. 10.1016/j.geomorph.2015.10.023
- Summer rainfall dissolved organic carbon, solute, and sediment fluxes in a small Arctic coastal catchment on Herschel Island (Yukon Territory, Canada) C. Coch et al. 10.1139/as-2018-0010
- Collapsing Arctic coastlines M. Fritz et al. 10.1038/nclimate3188
- Linkages Among Climate, Fire, and Thermoerosion in Alaskan Tundra Over the Past Three Millennia M. Chipman & F. Hu 10.1002/2017JG004027
- TerraSAR-X Time Series Fill a Gap in Spaceborne Snowmelt Monitoring of Small Arctic Catchments—A Case Study on Qikiqtaruk (Herschel Island), Canada S. Stettner et al. 10.3390/rs10071155
16 citations as recorded by crossref.
- Prokaryotic community in Pleistocene ice wedges of Mammoth Mountain A. Rakitin et al. 10.1007/s00792-019-01138-z
- Sedimentary and geochemical characteristics of two small permafrost-dominated Arctic river deltas in northern Alaska M. Fuchs et al. 10.1007/s41063-018-0056-9
- Eroding permafrost coasts release low amounts of dissolved organic carbon (DOC) from ground ice into the nearshore zone of the Arctic Ocean G. Tanski et al. 10.1002/2015GB005337
- Ice wedges as archives of winter paleoclimate: A review T. Opel et al. 10.1002/ppp.1980
- Holocene ice-wedge polygon development in northern Yukon permafrost peatlands (Canada) M. Fritz et al. 10.1016/j.quascirev.2016.02.008
- Dissolved organic carbon in permafrost regions: A review Q. Ma et al. 10.1007/s11430-018-9309-6
- Reviews and syntheses: Effects of permafrost thaw on Arctic aquatic ecosystems J. Vonk et al. 10.5194/bg-12-7129-2015
- Reviews and Syntheses: Effects of permafrost thaw on arctic aquatic ecosystems J. Vonk et al. 10.5194/bgd-12-10719-2015
- Variability in transport of terrigenous material on the shelves and the deep Arctic Ocean during the Holocene C. Wegner et al. 10.3402/polar.v34.24964
- Deep Yedoma permafrost: A synthesis of depositional characteristics and carbon vulnerability J. Strauss et al. 10.1016/j.earscirev.2017.07.007
- Transformation of terrestrial organic matter along thermokarst-affected permafrost coasts in the Arctic G. Tanski et al. 10.1016/j.scitotenv.2016.12.152
- Retrogressive thaw slumps temper dissolved organic carbon delivery to streams of the Peel Plateau, NWT, Canada C. Littlefair et al. 10.5194/bg-14-5487-2017
- Patterns and rates of riverbank erosion involving ice-rich permafrost (yedoma) in northern Alaska M. Kanevskiy et al. 10.1016/j.geomorph.2015.10.023
- Summer rainfall dissolved organic carbon, solute, and sediment fluxes in a small Arctic coastal catchment on Herschel Island (Yukon Territory, Canada) C. Coch et al. 10.1139/as-2018-0010
- Collapsing Arctic coastlines M. Fritz et al. 10.1038/nclimate3188
- Linkages Among Climate, Fire, and Thermoerosion in Alaskan Tundra Over the Past Three Millennia M. Chipman & F. Hu 10.1002/2017JG004027
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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.
Ground ice in permafrost has not, until now, been considered to be a source of dissolved organic...
The Cryosphere
An interactive open-access journal of the European Geosciences Union
