Advances in Atmospheric Sciences

, Volume 30, Issue 5, pp 1449–1460

Impact of rain snow threshold temperature on snow depth simulation in land surface and regional atmospheric models

Authors

    • Key Laboratory of Land Surface Process and Climate Change in Cold and Arid Regions, Cold and Arid Regions Environmental and Engineering Research InstituteChinese Academy of Sciences
    • Laboratory of Arid Climatic Changing and Reducing Disaster of Gansu Province, Cold and Arid Regions Environmental and Engineering Research InstituteChinese Academy of Sciences
  • Nidhi Nagabhatla
    • Institut für UmweltplanungGottfried Wilhelm Leibniz Universität
  • Shihua Lü吕世华
    • Key Laboratory of Land Surface Process and Climate Change in Cold and Arid Regions, Cold and Arid Regions Environmental and Engineering Research InstituteChinese Academy of Sciences
  • Shih-Yu Wang
    • Department of Plants, Soils, and ClimateUtah State University
Article

DOI: 10.1007/s00376-012-2192-7

Cite this article as:
Wen, L., Nagabhatla, N., Lü, S. et al. Adv. Atmos. Sci. (2013) 30: 1449. doi:10.1007/s00376-012-2192-7
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Abstract

This study investigates the impact of rain snow threshold (RST) temperatures on snow depth simulation using the Community Land Model (CLM) and the Weather Research and Forecasting model (WRF—coupled with the CLM and hereafter referred to as WRF_CLM), and the difference in impacts. Simulations were performed from 17 December 1994 to 30 May 1995 in the French Alps. Results showed that both the CLM and the WRF_CLM were able to represent a fair simulation of snow depth with actual terrain height and 2.5°C RST temperature. When six RST methods were applied to the simulation using WRF_CLM, the simulated snow depth was the closest to observations using 2.5°C RST temperature, followed by that with Pipes’, USACE, Kienzle’s, Dai’s, and 0°C RST temperature methods. In the case of using CLM, simulated snow depth was the closest to the observation with Dai’s method, followed by with USACE, Pipes’, 2.5°C RST temperature, Kienzle’s, and 0°C RST temperature method. The snow depth simulation using the WRF_CLM was comparatively sensitive to changes in RST temperatures, because the RST temperature was not only the factor to partition snow and rainfall. In addition, the simulated snow related to RST temperature could induce a significant feedback by influencing the meteorological variables forcing the land surface model in WRF_CLM. In comparison, the above variables did not change with changes in RST in CLM. Impacts of RST temperatures on snow depth simulation could also be influenced by the patterns of temperature and precipitation, spatial resolution, and input terrain heights.

Key words

snow simulationRST temperatureWRF_CLMCLM
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© Chinese National Committee for International Association of Meteorology and Atmospheric Sciences, Institute of Atmospheric Physics, Science Press and Springer-Verlag Berlin Heidelberg 2013