...
首页> 外文期刊>TAO: Terrastrial, atmospheric, and oceanic sciences >The Effects of the Heavy Rainfall Event of 12 June 2005 on Taiwan Terrain
【24h】

The Effects of the Heavy Rainfall Event of 12 June 2005 on Taiwan Terrain

机译:2005年6月12日的强降雨事件对台湾地形的影响

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

A series of numerical simulations are conducted using the Weather Research and Forecasting (WRF-ARW) model with a 9-km mesh to examine the physical processes responsible for the torrential rainfall associated with a mesoscale convective system (MCS) along the Mei-Yu front that caused severe damage over southwestern Taiwan on 12 June 2005. In the control experiment (with full Taiwan terrain), the MCS tends to propagate northward along the windward (western) slope, rather than being advected downstream, as it encounters the southern Central Mountain Range (CMR). The low-level convergence between the dynamically-driven return flow and the incoming southwesterly flow is an important factor for the northward propagation of the MCS. The values of the unsaturated moist Froude number (F_w) and the convective available potential energy (CAPE) are about 0.333 and 2858 J kg~(-1) for the convectively unstable basic flow. This airflow belongs to the flow-around regime as suggested by previous studies. In this flow regime, the torrential rainfall associated with the simulated MCS occurs on both the upslope side and adjacent plains over southwestern Taiwan, which agrees well with the observed rainfall distribution. A sensitivity study of lowering the Taiwan terrain elevations to 80% (F_w~0.416) or 60% (F_w~0.555) of that in the control experiment reveals that the airflow is characterized by a long-lasting orographic convective system near the mountain peaks. The simulated torrential rainfall mainly occurs along the mountain peaks of the southern CMR. The experiment with a reduced elevation to 40% (F_w~0.833) or 20% (F_w~1.666) in the control experiment shows a downstream-propagating MCS, which falls into the flow-over regime. This study demonstrates that the northward propagating MCS, which is mainly caused by the flow deflection by southern CMR, played a key role in producing torrential rainfall over southwestern Taiwan during 0000 -1200 UTC 12 June 2005.
机译:使用带有9公里网格的天气研究和预报(WRF-ARW)模型进行了一系列数值模拟,以检查与梅雨锋前中尺度对流系统(MCS)相关的暴雨的物理过程在2005年6月12日对台湾西南部地区造成了严重破坏。在控制实验(具有完整的台湾地形)中,MCS倾向于沿顺风(西)坡向北传播,而不是在遇到南部中央山脉时向下游平流。范围(CMR)。在动态驱动的回流与进入的西南风之间的低水平收敛是MCS向北传播的重要因素。对流不稳定基流的非饱和湿弗洛德数(F_w)和对流可用势能(CAPE)分别约为0.333和2858 J kg〜(-1)。如先前的研究所建议的,这种气流属于绕流状态。在这种流态下,与模拟MCS相关的暴雨发生在台湾西南部的上坡侧和相邻平原上,这与观测到的降雨分布非常吻合。通过将台湾地形海拔降低到对照实验中的80%(F_w〜0.416)或60%(F_w〜0.555)的敏感性研究表明,气流的特征在于山峰附近的地形对流系统持久。模拟的暴雨主要发生在CMR南部的山峰上。在控制实验中,将标高降低到40%(F_w〜0.833)或20%(F_w〜1.666)的实验显示,下游传播的MCS属于流溢状态。这项研究表明,向南传播的MCS主要是由南部CMR的流量偏转引起的,它在2005年6月12日0000 -1200 UTC期间在台湾西南部产生暴雨中起了关键作用。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号