青藏高原隆升作用于大气临界高度的数值研究

NUMERICAL STUDIES ON THE EFFECTS OF THE CRITICAL HEIGHT OF QINGHAI-XIZANG PLATEAU UPLIFT ON THE ATMOSPHERE

  • 摘要: 利用P-σ混合坐标系全球大气环流模式研究了青藏高原隆升作用于大气临界高度问题,通过对数值试验结果的分析进一步证实了在高原隆升的过程中存在着一个临界高度,这个高度在夏季约为1500~2000m.当高原总体平均高度超过临界高度后,高原周围地区的气流主要以绕流为主,爬坡气流的速度较小,稳定的高原季风开始形成,高原地区范围内为强大的上升运动区,高原南侧和中国东部地区出现一条明显的雨带,随着高原隆升高度的增高,雨带内的降水量逐渐增加,同时高原西侧附近地区形成一个稳定的感热通量大值带

     

    Abstract: The effects of the critical height of Qing hai-Xizang Plateau uplift on the atmosphere have been studied by using P-σ incorporated coordinate general circulation model system in this paper. Numerical experiment results show that there is a critical height during the course of Qinghai-Xizang Plateau uplift, which is near 1.5 km in summer. When the average height of the Plateau uplifting surpasses this critical height, a series of changes in general circulation and climatic elements will occur. The uplift of the Plateau changes the air flow pattern ar ound the Plateau. The deep and steady Plateau monsoon appears. There are maximum sensible centers over the western Plateau. The rainbelt and precipitation amount will be also changed obviously.

     

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