Development and Application of Improved Double Layer Snow-Melting Model in Changing Environment

Article Preview

Abstract:

Climate change is a hot issue on the current time and snow melting process in alpine areas has be affected on the background of climate change, so it is necessary to study snow melting process especially the snowmelt model. In view of the shortcomings of the degree-day model (DDM), the double layer snow-melt model (DSMM) is improved and developed based on the original theory. Then the simulation of the snowmelt process of the upper reaches of Lancang-Mekong River is performed by the improved double layer snow-melt model (IDSMM) and DDM respectively, the simulation results are analyzed in view of model theory, snowmelt critical control conditions, the effects of the simulation and working conditions in the changing environment. The results show that IDSMM based on the energy and mass balance is superior to DDM in the snowmelt physics mechanism, and it not only can simulate the snow melting process, but also can simulate many physical processes, such as the canopy interception of snowfall, vaporization and sublimation loss in evaporation, the second precipitation from canopy surface, the process of snowmelt water freezing again and so on. The simulation results of snowmelt process is more tally with the actual situation and it can provide a reference to the research of snow and ice hydrology and the whole water cycle in a changing environment.

You might also be interested in these eBooks

Info:

Periodical:

Advanced Materials Research (Volumes 1065-1069)

Pages:

3260-3266

Citation:

Online since:

December 2014

Export:

Price:

Permissions CCC:

Permissions PLS:

Сopyright:

© 2015 Trans Tech Publications Ltd. All Rights Reserved

Share:

Citation:

* - Corresponding Author

[1] Xiong Li-hua, Guo Sheng-lian, 2004. Distributed Watershed Hydrologic Model[M]. China WaterPower Press, 184-187.

Google Scholar

[2] MU Zhen-xia, JIANG Hu-i fang, 2010. The Ef fects of Global Climate Change on Snowmel-t runoffs in High Cold Alpine Areas and a Sensitivity Analysis of Them. China Rural Water and Hydropower, 8-15.

Google Scholar

[3] Houghton J, Meira Filho L, Callander B, et al. Climate Change 1995: The Science of Climate Change[ M] . Cambridge University Press, (1996).

Google Scholar

[4] Mccarthy J J , Working G I. Climate Change 2001: Impacts, Adaptation, and Vulnerability [ M ] . Cambridge University Press New York , (2001).

Google Scholar

[5] Hu S S, Liu C M, Zheng H X et al., 2012. Assessing the impacts of climate variability and human activities on streamflow in the water source area of Baiyangdian Lake. Journal of Geographical Sciences, 22(5): 895−905.

DOI: 10.1007/s11442-012-0971-9

Google Scholar

[6] P.G. Clem, M. Rodriguez, J.A. Voigt and C.S. Ashley, U.S. Patent 6, 231, 666. (2001).

Google Scholar

[7] Immerzeel W W, van Beek L P H, Bierkens M F P, 2010. Climate change will affect the Asian Water Towers. Science, 328: 1382−1385.

DOI: 10.1126/science.1183188

Google Scholar

[8] Jiang F Q, Hu R J, Zhang Y W et al., 2011. Variations and trends of onset, cessation and length of climatic growing season over Xinjiang, NW China. Theoretical and Applied Climatology, 106: 449−458.

DOI: 10.1007/s00704-011-0445-5

Google Scholar

[9] Langlois J L, Johnson D W, Mehuys G R, 2005. Suspended sediment dynamics associated with snowmelt runoff in a small mountain stream of Lake Tahoe (Nevada). Hydrological Processes, 19(18): 3569−3580.

DOI: 10.1002/hyp.5844

Google Scholar

[10] Lilbaek G, Pomeroy J W, 2008. Ion enrichment of snowmelt runoff water caused by basal ice formation. Hydrological Processes, 22(15): 2758−2766.

DOI: 10.1002/hyp.7028

Google Scholar