Articles | Volume 9, issue 2
https://doi.org/10.5194/tc-9-719-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-9-719-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Future permafrost conditions along environmental gradients in Zackenberg, Greenland
S. Westermann
Center for Permafrost (CENPERM), Department of Geosciences and Natural Resource Management, University of Copenhagen, Øster Voldgade 10, 1350 Copenhagen K., Denmark
Department of Geosciences, University of Oslo, P.O. Box 1047, Blindern, 0316 Oslo, Norway
Center for Permafrost (CENPERM), Department of Geosciences and Natural Resource Management, University of Copenhagen, Øster Voldgade 10, 1350 Copenhagen K., Denmark
S. Højlund Pedersen
Department of Bioscience – Arctic Research Centre, Aarhus University, Frederiksborgvej 399, 4000 Roskilde, Denmark
M. Stendel
Danish Climate Centre – Danish Meteorological Institute, Lyngbyvej 100, 2100 Copenhagen, Denmark
B. U. Hansen
Center for Permafrost (CENPERM), Department of Geosciences and Natural Resource Management, University of Copenhagen, Øster Voldgade 10, 1350 Copenhagen K., Denmark
G. E. Liston
Cooperative Institute for Research in the Atmosphere, Colorado State University, 1375 Campus Delivery, Fort Collins, CO 80523-1375, USA
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- Northern Hemisphere permafrost map based on TTOP modelling for 2000–2016 at 1 km2 scale J. Obu et al. 10.1016/j.earscirev.2019.04.023
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- Modelling present and future permafrost thermal regimes in Northeast Greenland L. Rasmussen et al. 10.1016/j.coldregions.2017.10.011
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Short summary
The development of ground temperatures in permafrost areas is influenced by many factors varying on different spatial and temporal scales. We present numerical simulations of ground temperatures for the Zackenberg valley in NE Greenland, which take into account the spatial variability of snow depths, surface and ground properties at a scale of 10m. The ensemble of the model grid cells suggests a spatial variability of annual average ground temperatures of up to 5°C.
The development of ground temperatures in permafrost areas is influenced by many factors varying...