An extension of the force-restore method to estimating soil temperature at depth and evaluation for frozen soils under snow
The force‐restore method (FRM) was originally developed for estimating diurnal fluctuations in the ground surface temperature. Because of its relatively simple parameterization, it is commonly applied in meteorological and other models for this purpose. Its application to the calculation of deeper s...
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Veröffentlicht in: | Journal of Geophysical Research. D. Atmospheres 2002-12, Vol.107 (D24), p.ACL 11-1-ACL 11-10 |
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