不同地形资料对西南涡降水过程的数值模拟研究

Numerical Simulation Study on Southwest Vortex Precipitation Processes by Using Different Terrain Data

  • 摘要: 本文仅改变模式下垫面的地形资料,对西南地区降水过程进行模拟试验,通过模拟结果的分析对比,我们认为1)不同地形资料(或是对地形资料进行平滑处理),在地形突变处的差异最为显著。2)地形细微的变化最直接影响的是降水位置,其次是降水强度。3)地形变化之后,短波辐射受到的影响最为直接,感热通量和潜热通量是此消彼长。4)盆地有降水过程时,低层一般盛行东南风,且会在盆地内部产生气旋性弯曲,气流在迎风坡存在明显的辐合,而背风坡则存在明显的辐散。5)地形梯度同样影响对流的发生发展,在地形陡峭处更容易产生强烈的上升运动,地形梯度越缓,气流的爬升能力也越强。总之,地形的微小变化已经可以对降水的落区和强度产生显著的影响。

     

    Abstract: A numerical modeling of precipitation in the south area is conducted just by changing the terrain data of underlying surface.The simulation results are as follows: 1) The difference is the most significant in a sudden change of terrain.2) The location and secondly intensity of precipitation are effected directly by the tiny change of terrain.3) The shortwave radiation is influenced directly when the terrain is changed,and sensible /latent heat fluxes eliminate and replace each other.4) When there is precipitation in Sichuan Basin,a southeast wind prevails in the lower layer and can result in cyclonic curvature in the basin.Convergence will remarkably occur in the windward slope and divergence in the leeward slope.5) Terrain gradient also influence the development of convection.The ascending motion occurs much easier in the steep terrain and the milder the slope,the more powerfully the current climbs.In a word,a tiny change of terrain can already influence the location and the intensity of precipitation obviously.

     

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