山地对积云的影响数值模拟
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NUMERICAL MODELING OF THE EFFECTS OF MOUNTAINS ON WARM CUMULUS CLOUDS
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    摘要:

    使用二维平面对称暖积云模式模拟了三种理想地形对随坏境风移动的积云的作用,试验了山地处理技术,计算结果与观测事实比较一致。结果表明,积云移过孤立山地或移入山区时受到增强,雨量增大;而移出山地的积云则被减弱。地形作用在积云发展初期较明显。山地表面加热形成的山地环流回流下沉运动区对向山地靠拢的积云有一定削弱作用。

    Abstract:

    The effects of three ideal types of terrain on clouds which move with ambient wind have been simulated by using a two-dimensional slab-symmetric warm cloud model. A simple technique of terrain processing is used. And the results of this modeling are fairly consistent with observations.The modeled clouds moving over isolate mountains or into mountain areas undergo some enhancement, with larger amount of rainfall, whereas those moving out of mountain areas become weakened a lot. The effect of terrains is more obvious in the early developing stage of the clouds.The downdraft of the local circulation formed because of the heating of the mountain slope has a slight negative effect on the development of the approaching clouds.

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孔凡铀,黄美元,徐华英,1988.山地对积云的影响数值模拟[J].大气科学学报,11(2):144-151. Kong Fanyou, Huang Meiyuan, Xu Huaying,1988. NUMERICAL MODELING OF THE EFFECTS OF MOUNTAINS ON WARM CUMULUS CLOUDS[J]. Trans Atmos Sci,11(2):144-151.

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  • 收稿日期:1986-12-03
  • 最后修改日期:1987-04-06
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