globalchange  > 气候变化与战略
DOI: 10.5194/hess-24-4813-2020
论文题名:
Understanding the mass; momentum; and energy transfer in the frozen soil with three levels of model complexities
作者: Yu L.; Zeng Y.; Su Z.
刊名: Hydrology and Earth System Sciences
ISSN: 1027-5606
出版年: 2020
卷: 24, 期:10
起始页码: 4813
结束页码: 4830
语种: 英语
Scopus关键词: Earth (planet) ; Energy transfer ; Flow of water ; Frozen soils ; Heat flux ; Latent heat ; Mass transfer ; Momentum ; Soil moisture ; Changing climate ; Coupled heat and mass transfer ; Heat and mass transfer models ; Model complexity ; Model performance ; Simultaneous transfer ; Surface latent heat fluxes ; Transition period ; Heat transfer performance ; atmospheric pressure ; climate change ; complexity ; frozen ground ; ground cover ; heat budget ; heat transfer ; latent heat flux ; meadow ; model ; soil temperature
英文摘要: Frozen ground covers a vast area of the Earth’s surface and it has important ecohydrological implications for cold 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 Simultaneous Transfer of Mass, Momentum, and Energy in Unsaturated Soil (STEMMUS), the complexity of the soil heat and mass transfer model varies from the basic coupled model (termed BCM) to the advanced coupled heat and mass transfer model (ACM), and, furthermore, to the explicit consideration of airflow (ACM–AIR). The impact of different model complexities on understanding the mass, momentum, and energy transfer in frozen soil was investigated. The model performance in simulating water and heat transfer and surface latent heat flux was evaluated over a typical Tibetan plateau meadow site. Results indicate that the ACM considerably improved the simulation of soil moisture, temperature, and latent heat flux. The analysis of the heat budget reveals that the improvement of soil temperature simulations by ACM is attributed to its physical consideration of vapor flow and the thermal effect on water flow, with the former mainly functioning above the evaporative front and the latter dominating below the evaporative front. The contribution of airflow-induced water and heat transport (driven by the air pressure gradient) to the total mass and energy fluxes is negligible. Nevertheless, given the explicit consideration of airflow, vapor flow and its effects on heat transfer were enhanced during the freezing–thawing transition period. © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License.
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被引频次[WOS]:28   [查看WOS记录]     [查看WOS中相关记录]
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/162578
Appears in Collections:气候变化与战略

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作者单位: Yu, L., Faculty of Geo-information Science and Earth Observation (ITC), University of Twente, Enschede, Netherlands; Zeng, Y., Faculty of Geo-information Science and Earth Observation (ITC), University of Twente, Enschede, Netherlands; Su, Z., Faculty of Geo-information Science and Earth Observation (ITC), University of Twente, Enschede, Netherlands, Key Laboratory of Subsurface Hydrology and Ecological Effect in Arid Region of Ministry of Education, School of Water and Environment, Chang’an University, Xi’an, China

Recommended Citation:
Yu L.,Zeng Y.,Su Z.. Understanding the mass; momentum; and energy transfer in the frozen soil with three levels of model complexities[J]. Hydrology and Earth System Sciences,2020-01-01,24(10)
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