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Hydrol. Earth Syst. Sci. Discuss., 6, 843-857, 2009
www.hydrol-earth-syst-sci-discuss.net/6/843/2009/
doi:10.5194/hessd-6-843-2009
© Author(s) 2009. This work is distributed
under the Creative Commons Attribution 3.0 License.


Snow distribution over the Namco lake area of the Tibetan Plateau

M. Li1, Y. Ma1,2, Z. Hu1, H. Ishikawa3, and Y. Oku3
1Cold and Arid Region Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
2Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China
3Disaster Prevention Research Institute, Kyoto University, Kyoto 611-0011, Japan

Abstract. The mesoscale snow distribution over the Namco lake area of the Tibetan Plateau on October 2005 has been investigated in this paper. The control and sensitive experiments were conducted using Weather Research Model (WRF) with three nested grids that included a 1 km finest grid centered on the Namco station. Our simulation ran from 6 October through 10 October 2005, which was concurrent with long term meteorological observations. Evaluation against boundary layer meteorological tower measurements and flux observations showed that the model captured the observed 2 m temperature and 10 m winds reasonably well in the sensitive experiment. The results suggested that output snow depth maximum amounts from two simulated experiments were centered downwind shore of Namco lake. Modified surface parameters for example surface skin temperature on the lake help to increase simulated credibility.

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Citation: Li, M., Ma, Y., Hu, Z., Ishikawa, H., and Oku, Y.: Snow distribution over the Namco lake area of the Tibetan Plateau, Hydrol. Earth Syst. Sci. Discuss., 6, 843-857, doi:10.5194/hessd-6-843-2009, 2009.   Bibtex   EndNote   Reference Manager    XML