Welcome to Chinese Journal of Applied Ecology! Today is Share:

Chinese Journal of Applied Ecology ›› 2018, Vol. 29 ›› Issue (2): 483-491.doi: 10.13287/j.1001-9332.201802.012

• Original Articles • Previous Articles     Next Articles

Capacity of Caragana microphylla shrub on counteracting snow movement and its influence on snow morphology in the Xilinhot Steppe, China.

YAN Min1, ZUO He-jun1*, DONG Zhi2, LIU Bao-he1, WANG Yan-jiao1, WEI Xiang-hong1, LI Gang-tie1   

  1. 1College of Desert Control Science and Engineering, Inner Mongolia Agricultural University/Inner Mongolia Key Laboratory of Aeolian Physics and Desertification Control Engineering, Hohhot 010011, China;
    2 College of Forestry, Shandong Agricultural University, Tai’an 271018, Shandong, China
  • Received:2017-06-28 Online:2018-02-18 Published:2018-02-18
  • Contact: E-mail: zuohj@126.com
  • Supported by:

    This work was supported by the National Natural Science Foundation of China (41361012).

Abstract: The aim of this study was to examine the impacts of characteristics of the shrub (shrub height, shrub width on the windward side, shrub length on the downwind side) on the snow morphology (snow height, snow width, and snow tail length) in the typical steppe of Xilinhot, China. The relationship between shrub height and parameters of snow morphology showed significant quadratic polynomial regression. The relationship between shrub width on the windward side, length on the downwind side and parameters of snow morphology showed significant power function (exponent was less than 1). The morphology and development characteristics of shrub snow were affected by the shrub characteristic parameters. Shrub height had the greatest influence on snow height. Shrub width at the windward side had the greatest influence on snow width and snow tail length. The snow morphology developed faster when the shrub was small, and then tended to be stable. The two-dimensional snow retention range model of shrub directly reflected the disturbance range of shrub to wind and the potential range of snow, indirectly reflected the capacity of shrub to retard snow movement. The three-dimensional snow blocking volume model of shrub snow directly reflected the snow resistance capacity of shrub under certain snow sources and wind conditions. Both models established here would provide a theoretical basis for estimating snow resources and preventing snow disaster in the wind blown snow area of typical steppe.