Articles | Volume 24, issue 10
Hydrol. Earth Syst. Sci., 24, 4813–4830, 2020
https://doi.org/10.5194/hess-24-4813-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue: Data acquisition and modelling of hydrological, hydrogeological...
Hydrol. Earth Syst. Sci., 24, 4813–4830, 2020
https://doi.org/10.5194/hess-24-4813-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
12 Oct 2020
Research article
| 12 Oct 2020
Understanding the mass, momentum, and energy transfer in the frozen soil with three levels of model complexities
Lianyu Yu et al.
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Cited
15 citations as recorded by crossref.
- Development of the Hydrus-1D freezing module and its application in simulating the coupled movement of water, vapor, and heat C. Zheng et al. 10.1016/j.jhydrol.2021.126250
- Monitoring Water and Energy Cycles at Climate Scale in the Third Pole Environment (CLIMATE-TPE) Z. Su et al. 10.3390/rs13183661
- Chemical characteristics of salt migration in frozen soils during the freezing-thawing period M. Wang et al. 10.1016/j.jhydrol.2021.127403
- The role of vadose zone physics in the ecohydrological response of a Tibetan meadow to freeze–thaw cycles L. Yu et al. 10.5194/tc-14-4653-2020
- Factors controlling the rise and fall of groundwater level during the freezing-thawing period in seasonal frozen regions H. Lyu et al. 10.1016/j.jhydrol.2022.127442
- STEMMUS-UEB v1.0.0: integrated modeling of snowpack and soil water and energy transfer with three complexity levels of soil physical processes L. Yu et al. 10.5194/gmd-14-7345-2021
- Interaction of soil water and groundwater during the freezing–thawing cycle: field observations and numerical modeling H. Xie et al. 10.5194/hess-25-4243-2021
- A novel model of heat-water-air-stress coupling in unsaturated frozen soil Z. Li et al. 10.1016/j.ijheatmasstransfer.2021.121375
- Convective heat transfer of spring meltwater accelerates active layer phase change in Tibet permafrost areas Y. Zhao et al. 10.5194/tc-16-825-2022
- Predicting the Soil Freezing Characteristic From the Particle Size Distribution Based on Micro‐Pore Space Geometry C. Wang et al. 10.1029/2021WR030782
- Soil hydrothermal modeling in a dry alpine agricultural zone: The effect of soil airflow J. Wang et al. 10.1016/j.geoderma.2021.115354
- A new seasonal frozen soil water-thermal coupled migration model and its numerical simulation C. Zhang et al. 10.1371/journal.pone.0258861
- Effect of increasing rainfall on the thermal—moisture dynamics of permafrost active layer in the central Qinghai—Tibet Plateau Z. Zhou et al. 10.1007/s11629-021-6707-5
- Improvement of summer precipitation simulation in China by assimilating spring soil moisture over the Tibetan Plateau J. Shen et al. 10.1007/s00704-021-03840-5
- New measures of deep soil water recharge during the vegetation restoration process in semi-arid regions of northern China Y. Cheng et al. 10.5194/hess-24-5875-2020
15 citations as recorded by crossref.
- Development of the Hydrus-1D freezing module and its application in simulating the coupled movement of water, vapor, and heat C. Zheng et al. 10.1016/j.jhydrol.2021.126250
- Monitoring Water and Energy Cycles at Climate Scale in the Third Pole Environment (CLIMATE-TPE) Z. Su et al. 10.3390/rs13183661
- Chemical characteristics of salt migration in frozen soils during the freezing-thawing period M. Wang et al. 10.1016/j.jhydrol.2021.127403
- The role of vadose zone physics in the ecohydrological response of a Tibetan meadow to freeze–thaw cycles L. Yu et al. 10.5194/tc-14-4653-2020
- Factors controlling the rise and fall of groundwater level during the freezing-thawing period in seasonal frozen regions H. Lyu et al. 10.1016/j.jhydrol.2022.127442
- STEMMUS-UEB v1.0.0: integrated modeling of snowpack and soil water and energy transfer with three complexity levels of soil physical processes L. Yu et al. 10.5194/gmd-14-7345-2021
- Interaction of soil water and groundwater during the freezing–thawing cycle: field observations and numerical modeling H. Xie et al. 10.5194/hess-25-4243-2021
- A novel model of heat-water-air-stress coupling in unsaturated frozen soil Z. Li et al. 10.1016/j.ijheatmasstransfer.2021.121375
- Convective heat transfer of spring meltwater accelerates active layer phase change in Tibet permafrost areas Y. Zhao et al. 10.5194/tc-16-825-2022
- Predicting the Soil Freezing Characteristic From the Particle Size Distribution Based on Micro‐Pore Space Geometry C. Wang et al. 10.1029/2021WR030782
- Soil hydrothermal modeling in a dry alpine agricultural zone: The effect of soil airflow J. Wang et al. 10.1016/j.geoderma.2021.115354
- A new seasonal frozen soil water-thermal coupled migration model and its numerical simulation C. Zhang et al. 10.1371/journal.pone.0258861
- Effect of increasing rainfall on the thermal—moisture dynamics of permafrost active layer in the central Qinghai—Tibet Plateau Z. Zhou et al. 10.1007/s11629-021-6707-5
- Improvement of summer precipitation simulation in China by assimilating spring soil moisture over the Tibetan Plateau J. Shen et al. 10.1007/s00704-021-03840-5
- New measures of deep soil water recharge during the vegetation restoration process in semi-arid regions of northern China Y. Cheng et al. 10.5194/hess-24-5875-2020
Latest update: 29 Jan 2023
Short summary
Soil mass and heat transfer processes were represented in three levels of model complexities to understand soil freeze–thaw mechanisms. Results indicate that coupled mass and heat transfer models considerably improved simulations of the soil hydrothermal regime. Vapor flow and thermal effects on water flow are the main mechanisms for the improvements. Given the explicit consideration of airflow, vapor flow and its effects on heat transfer were enhanced during the freeze–thaw transition period.
Soil mass and heat transfer processes were represented in three levels of model complexities to...
