Difference between revisions of "Soil Thermal Conduction in the Generic PCM"
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LucasLange (talk | contribs) (Created page with "== Purpose == The goal of this page is to summarize key aspects, both theoretical and practical, of the computation of subsurface temperatures in the generic PCM. == Theoret...") |
LucasLange (talk | contribs) (→Theoretical Considerations) |
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== Theoretical Considerations == | == Theoretical Considerations == | ||
| − | The computation of the heat conduction in the soil was based on the 1D layer soil model originally described by | + | The computation of the heat conduction in the soil was based on the 1D layer soil model originally described by Hourdin et al. (2013). Since that, E. Millour modified this scheme to include the possibility of varying the thermal properties with depth. |
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| + | == References == | ||
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| + | Hourdin, F., Van, P. L., Forget, F., and Talagrand, O. (1993). Meteorological variability and the annual surface pressure cycle on Mars. Journal of Atmospheric Sciences, 50(21):3625 – 3640. | ||
== References == | == References == | ||
Revision as of 09:55, 5 March 2025
Purpose
The goal of this page is to summarize key aspects, both theoretical and practical, of the computation of subsurface temperatures in the generic PCM.
Theoretical Considerations
The computation of the heat conduction in the soil was based on the 1D layer soil model originally described by Hourdin et al. (2013). Since that, E. Millour modified this scheme to include the possibility of varying the thermal properties with depth.
References
Hourdin, F., Van, P. L., Forget, F., and Talagrand, O. (1993). Meteorological variability and the annual surface pressure cycle on Mars. Journal of Atmospheric Sciences, 50(21):3625 – 3640.
