A copy of this work was available on the public web and has been preserved in the Wayback Machine. The capture dates from 2020; you can also visit the original URL.
The file type is application/pdf
.
Understanding the Mass, Momentum and Energy Transfer in the Frozen Soil with Three Levels of Model Complexities
[post]
2020
unpublished
Abstract. Frozen ground covers vast area of earth surface and has its important ecohydrological implications for high latitude and high altitude regions under changing climate. However, it is challenging to characterize the simultaneous transfer of mass and energy in frozen soils. Within the modeling framework of STEMMUS (Simultaneous Transfer of Mass, Momentum and Energy in Unsaturated Soil), the model complexity of soil heat and mass transfer varies from uncoupled, to coupled heat and mass
doi:10.5194/hess-2020-253
fatcat:q2caajbzwnfplkzpy23ywtneiu