Articles | Volume 19, issue 8
https://doi.org/10.5194/gmd-19-3509-2026
https://doi.org/10.5194/gmd-19-3509-2026
Model description paper
 | 
29 Apr 2026
Model description paper |  | 29 Apr 2026

Impact of soil heterogeneity and lateral heat fluxes on soil temperature simulations in a permafrost-affected soil

Melanie Alexandra Thurner, Xavier Rodriguez-Lloveras, and Christian Beer

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Cited articles

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Aas, K. S., Martin, L., Nitzbon, J., Langer, M., Boike, J., Lee, H., Berntsen, T. K., and Westermann, S.: Thaw processes in ice-rich permafrost landscapes represented with laterally coupled tiles in a land surface model, The Cryosphere, 13, 591–609, https://doi.org/10.5194/tc-13-591-2019, 2019. a, b, c, d, e, f, g, h, i, j, k
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Beer, C.: The Arctic carbon count, Nat. Geosci., 1, 569–570, 2008. a
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Short summary
Soil texture varies over centimeters, which is overseen by large-scale models, likely causing simulation errors. We developed a 2-dimesional geophysical soil model (DynSoM-2D) with a resolution of 10 cm and ran it with different setups at a permafrost-affected site. Using high-resolution input, DynSoM-2D simulates a warmer soil, which thaws deeper and has an extended snow-free period in summer. These changes can impact ecosystem dynamics, but have little effect on yearly soil-air heat exchange.
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