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Evaluation of Ten Fresh Snow Density Parameterization Schemes for Simulating Snow Depth and Surface Energy Fluxes on the Eastern Tibetan Plateau

Snow cover on the Tibetan Plateau has a shallow depth, plaque distribution, and repeated ablation. The applicability of the snow parameterization scheme in the current land surface process model on the TP needs to be further tested using observational data. In this paper, using the land surface proc...

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Published in:Atmosphere 2023-10, Vol.14 (10), p.1571
Main Authors: Li, Wenjing, Luo, Siqiong, Wang, Jingyuan, Wang, Yuxuan
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description Snow cover on the Tibetan Plateau has a shallow depth, plaque distribution, and repeated ablation. The applicability of the snow parameterization scheme in the current land surface process model on the TP needs to be further tested using observational data. In this paper, using the land surface process model CLM4.5 and ten fresh snow density parameterization schemes characterized by temperature, wind speed, and relative humidity, three discontinuous snow processes in Maqu, Madoi, and Yakou and two continuous snow processes in Madoi and Yakou were simulated. By comparing the simulated snow depth with the observed, it was found that this model can clearly describe repeated snow accumulation and ablation processes for the discontinuous snow cover process. The KW scheme, compared with the original Anderson scheme, performed the best regarding snow depth simulation. However, all schemes overestimated the melting rate of snow, and were not able to simulate continuous snow accumulation. The simulation effect of the Schmucki scheme on radiation and energy flux under discontinuous snow cover was significantly improved compared with other scheme. None of schemes performed perfectly, so future studies that focus on the simulations of snow depth, radiation flux, and energy flux under continuous snow cover for accurate and wide applications are recommended.
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The applicability of the snow parameterization scheme in the current land surface process model on the TP needs to be further tested using observational data. In this paper, using the land surface process model CLM4.5 and ten fresh snow density parameterization schemes characterized by temperature, wind speed, and relative humidity, three discontinuous snow processes in Maqu, Madoi, and Yakou and two continuous snow processes in Madoi and Yakou were simulated. By comparing the simulated snow depth with the observed, it was found that this model can clearly describe repeated snow accumulation and ablation processes for the discontinuous snow cover process. The KW scheme, compared with the original Anderson scheme, performed the best regarding snow depth simulation. However, all schemes overestimated the melting rate of snow, and were not able to simulate continuous snow accumulation. The simulation effect of the Schmucki scheme on radiation and energy flux under discontinuous snow cover was significantly improved compared with other scheme. None of schemes performed perfectly, so future studies that focus on the simulations of snow depth, radiation flux, and energy flux under continuous snow cover for accurate and wide applications are recommended.</description><identifier>ISSN: 2073-4433</identifier><identifier>EISSN: 2073-4433</identifier><identifier>DOI: 10.3390/atmos14101571</identifier><language>eng</language><publisher>Basel: MDPI AG</publisher><subject>Ablation ; Accumulation ; CLM4.5 ; Cold ; Density ; Depth ; Energy ; Energy flux ; Energy transfer ; Environmental aspects ; Fluctuations ; fresh snow density parameterization scheme ; Humidity ; Hydrology ; Ice ; Mountains ; Parameterization ; Precipitation ; Predation ; Radiation ; Radiation flux ; Relative humidity ; Simulation ; Snow ; Snow accumulation ; Snow cover ; Snow density ; Snow depth ; Summer ; Surface energy ; Surface properties ; Temperature ; Tibetan Plateau (TP) ; Wind speed ; Winter</subject><ispartof>Atmosphere, 2023-10, Vol.14 (10), p.1571</ispartof><rights>COPYRIGHT 2023 MDPI AG</rights><rights>2023 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). 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ispartof Atmosphere, 2023-10, Vol.14 (10), p.1571
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subjects Ablation
Accumulation
CLM4.5
Cold
Density
Depth
Energy
Energy flux
Energy transfer
Environmental aspects
Fluctuations
fresh snow density parameterization scheme
Humidity
Hydrology
Ice
Mountains
Parameterization
Precipitation
Predation
Radiation
Radiation flux
Relative humidity
Simulation
Snow
Snow accumulation
Snow cover
Snow density
Snow depth
Summer
Surface energy
Surface properties
Temperature
Tibetan Plateau (TP)
Wind speed
Winter
title Evaluation of Ten Fresh Snow Density Parameterization Schemes for Simulating Snow Depth and Surface Energy Fluxes on the Eastern Tibetan Plateau
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