Articles | Volume 12, issue 12
https://doi.org/10.5194/bg-12-3725-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/bg-12-3725-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Patterns and persistence of hydrologic carbon and nutrient export from collapsing upland permafrost
Department of Biology and Wildlife and Institute of Arctic Biology, University of Alaska Fairbanks, Fairbanks, USA
Observatoire des Sciences de l'Univers de Rennes (OSUR), UMR6553 ECOBIO-CNRS, University of Rennes 1, Rennes, France
J. B. Jones
Department of Biology and Wildlife and Institute of Arctic Biology, University of Alaska Fairbanks, Fairbanks, USA
S. E. Godsey
Department of Geosciences, Idaho State University, Pocatello, USA
J. R. Larouche
The Rubenstein School of Environment and Natural Resources, University of Vermont, Birmingham, USA
W. B. Bowden
The Rubenstein School of Environment and Natural Resources, University of Vermont, Birmingham, USA
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- Biogeochemistry of “pristine” freshwater stream and lake systems in the western Canadian Arctic J. Dean et al. 10.1007/s10533-016-0252-2
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- Trajectory of Topsoil Nitrogen Transformations Along a Thermo‐Erosion Gully on the Tibetan Plateau C. Mao et al. 10.1029/2018JG004805
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Short summary
As high latitudes warm, carbon and nitrogen stored in permafrost soil will be vulnerable to erosion and transport to Arctic streams and rivers. We sampled outflow from 83 permafrost collapse features in Alaska. Permafrost collapse caused substantial increases in dissolved organic carbon and inorganic nitrogen but decreased methane concentration by 90%. Upland thermokarst may be a dominant linkage transferring carbon and nutrients from terrestrial to aquatic ecosystems as the Arctic warms.
As high latitudes warm, carbon and nitrogen stored in permafrost soil will be vulnerable to...
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