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Volume 5, issue 3
The Cryosphere, 5, 741–757, 2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Modeling the spatial dynamics of permafrost and seasonally...

The Cryosphere, 5, 741–757, 2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 19 Sep 2011

Research article | 19 Sep 2011

Modeling the thermal dynamics of the active layer at two contrasting permafrost sites on Svalbard and on the Tibetan Plateau

J. Weismüller1,*, U. Wollschläger1,**,***, J. Boike2, X. Pan1, Q. Yu3, and K. Roth1 J. Weismüller et al.
  • 1Institute of Environmental Physics, Heidelberg University, Im Neuenheimer Feld 229, 69120 Heidelberg, Germany
  • 2Alfred Wegener Institute for Polar and Marine Research – Research Unit Potsdam, Telegrafenberg A 43, 14473 Potsdam, Germany
  • 3Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, 260 Donggang West Road, 730000 Lanzhou, China
  • *now at: Department of Earth and Environmental Sciences, Geophysics Section, Ludwig-Maximilians University, Theresienstr. 41, 80333 Munich, Germany
  • **now at: UFZ – Helmholtz Centre for Environmental Research, Permoserstr. 15, 04318 Leipzig, Germany
  • ***now at: WESS – Water and Earth System Science Competence Cluster, Keplerstr. 17, 72074 Tübingen, Germany

Abstract. Employing a one-dimensional, coupled thermal and hydraulic numerical model, we quantitatively analyze high-resolution, multi-year data from the active layers at two contrasting permafrost sites. The model implements heat conduction with the de Vries parameterization, heat convection with water and vapor flow, freeze-thaw transition parameterized with a heuristic soil-freezing characteristic, and liquid water flow with the Mualem-van Genuchten parameterization. The model is driven by measured temperatures and water contents at the upper and lower boundary with all required material properties deduced from the measured data. The aims are (i) to ascertain the applicability of such a rather simple model, (ii) to quantify the dominating processes, and (iii) to discuss possible causes of remaining deviations.

Soil temperatures and water contents as well as characteristic quantities like thaw depth and duration of the isothermal plateau could be reproduced. Heat conduction is found to be the dominant process by far at both sites, with non-conductive transport contributing a maximum of some 3% to the mean heat flux at the Spitsbergen site, most of the time very much less, and practically negligible at the Tibetan site. Hypotheses discussed to explain the remaining deviations between measured and simulated state variables include, besides some technical issues, infiltration of snow melt, dry cracking with associated vapor condensation, and mechanical soil expansion in detail.

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