Articles | Volume 19, issue 8
https://doi.org/10.5194/gmd-19-3509-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-19-3509-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Impact of soil heterogeneity and lateral heat fluxes on soil temperature simulations in a permafrost-affected soil
Melanie Alexandra Thurner
CORRESPONDING AUTHOR
Institute of Soil Science, University of Hamburg, Hamburg, Germany
KIT-Campus Alpin, Garmisch-Partenkirchen, Germany
Xavier Rodriguez-Lloveras
Institute of Soil Science, University of Hamburg, Hamburg, Germany
Christian Beer
CORRESPONDING AUTHOR
Institute of Soil Science, University of Hamburg, Hamburg, Germany
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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.
Soil texture varies over centimeters, which is overseen by large-scale models, likely causing...