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Large-scale Earth system and land surface … Large-scale Earth system and land surface models often lack an adequate representation of subgrid-scale processes in permafrost landscapes. Small-scale processes such as thermokarst formation might, however, considerably impact the energy and carbon budgets in way which is not resolved within large-scale models. Since a spatially high-resolved simulation of such processes is not feasible, novel techniques for up-scaling subgrid processes are demanded.</br>Within this work a one-dimensional model of the ground thermal regime of land surfaces, CryoGrid 3, is employed to conceptually represent small-scale features of permafrost landscapes, particularly those related to thermokarst. For example, the model has been shown to adequately describe the degradation of permafrost underneath waterbodies in a warming climate. Using tiling approaches such point-wise realizations can be up-scaled in a statistical way in order to represent larger land surface units.</br>The model development is closely linked to field campaigns to the Lena River Delta in Siberia which offers very diverse land surface features such as polygonal tundra and thermos-erosional valleys. These features are related to the region’s diverse soil stratigraphies, in particular the occurrence of ice-rich ground. Combining field measurements with modelling ultimately allows an improvement in the qualitative and quantitative understanding of the typical geomorphological processes in permafrost landscapes and their representation in large-scale land surface models.tation in large-scale land surface models. +
Towards representing thermokarst processes in land surface models +
Potsdam +
jan.nitzbon@awi.de +
Alfred Wegener Institute for Polar and Marine Research +
Nitzbon +
0049-331-288-2204 +
Image:Nitzbon_csdms_poster_A0_final.pdf +
Image:Nitzbon_csdms_poster_A0_final.png +
HPC workshop +
1) Bringing CSDMS models into the classroom +
1) Modeling Permafrost toolbox +
2) Introduction to EcoPath with Ecosim +
Germany +
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12:25:47, 6 March 2017 +
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17:25:44, 1 June 2017 +
