“8·31”云阳特大暴雨地形动力作用数值研究

Numerical Study of the Dynamic Effect of Terrain on“8.31”Extreme Torrential Rain in Yunyang

  • 摘要: 利用NCEP再分析资料和WRF模式对2014年8月31日云阳特大暴雨过程进行环流形势分析和数值模拟,并针对大巴山和齐岳山进行地形敏感性试验。结果表明:西南涡、辐合切变线、低空急流是本次暴雨的直接影响系统。大巴山对暴雨的影响主要是阻挡作用和迎风坡作用。大巴山高度降低后,低涡明显向北扩展,降水中心向东北方向偏移,低层辐合减弱导致垂直次级环流上升支强度和对流高度降低使暴雨减幅。齐岳山对暴雨的影响主要是地形狭管效应。齐岳山高度降低后,狭管效应减弱,低空急流强度减弱、位置南压;低层辐合区位置偏南导致垂直次级环流上升支的位置偏南。

     

    Abstract: Based on NCEP reanalysis data and WRF model,circulation feature analysis and numerical simulations are carried on for the extreme torrential rain in Yunyang on 31August,2014.In allusion to Daba mountains and Qiyue mountains,terrain sensitivity testsare designed.It is indicated that southwest vortex,shear line and low-level jet are the direct effect systems of this progress.The function of Daba mountains is obstruction and wind slope effect.With the reduction of the height of Daba mountains,low vortex move obviously northwards,precipitation cell move northeastwards,the weakening of low-level convergence brings about the weakening of intensity and ceiling of convection of the ascend branch of secondary verticalcirculation,which contributes to the decrease of the precipitation.The function of Qiyue mountains is funnelling.With the reduction of the height of Qiyue mountains,canalization minnished,low-level jet get weakend and move southwards,the position of low-level convergence move further south,which lead to the southward deflection of the ascend branch of secondary vertical circulation.

     

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