首页> 外文期刊>Atmospheric research >Numerical simulation and analysis of the Yangtze River Delta Rainstorm on 8 October 2013 caused by binary typhoons
【24h】

Numerical simulation and analysis of the Yangtze River Delta Rainstorm on 8 October 2013 caused by binary typhoons

机译:2013年10月8日长三角暴雨的数值模拟与分析。

获取原文
获取原文并翻译 | 示例
           

摘要

Torrential rainfall associated with the 23rd Typhoon Fitow in 2013 hit the Yangtze River Delta (YRD) region of China, resulting from mutual effects of residual low pressure cyclonic circulation of Fitow and the 24th Typhoon Danas, which imposed great challenge to forecasters. In this study, the Weather Research and Forecasting (WRF) model was used to simulate the rainstorm under the background of binary typhoons of Fitow and Danas. Three sensitivity experiments of typhoon intensity changes of binary typhoons were carried out. It was found that the Typhoon Danas was the main factor in this torrential rain event, in which its accompanied strong eastward low-level jet was the major moisture conveyor belt through which the warm and moist air was brought into the heavy rainfall zone and the static instability was maintained and enhanced over the YRD. The convergence line formed by periphery easterly flow of Typhoon Danas and southward cold air, together with the local frontogenesis mainly due to convergence, was an important trigger factor of this rainstorm. The large scale forcing was the major uplift mechanism, and the underlying frontal uplift played a secondary role for rainstorm in the north YRD, while uplift mechanism for rainstorm in the southern YRD is mainly local underlying frontal uplift induced large CAPE release resulting in local strong buoyancy uplift that led to strong upward motion. Not only did the convergence of twin typhoons directly provide dynamic conditions for the rainstorm, but also the dynamic lifting was enhanced by binary typhoons through strengthening the coupling of upper-level and low-level jet. The sensitivity tests revealed that the rainstorm in YRD was sensitive to both typhoons' intensity, and the rainfall in the south YRD was more sensitive than that in the north. A conceptual model of YRD rainstorm under binary typhoon situation was proposed based on the above-mentioned factors. (C) 2015 Elsevier B.V. All rights reserved.
机译:由于残存的菲托低压气旋环流和第24台风丹娜斯的相互影响,2013年第23台菲特飓风造成的强降雨袭击了中国的长江三角洲地区,这给预报员带来了巨大挑战。在这项研究中,使用了天气研究和预报(WRF)模型来模拟Fitow和Danas的二元台风背景下的暴雨。进行了三级台风强度变化的敏感性试验。人们发现,台风达纳斯是这次暴雨的主要因素,其伴随的强东风低空急流是主要的水分输送带,温暖潮湿的空气通过该输送带进入大雨量区和静水区。长期维持和增加了不稳定。台风达纳斯和南侧冷空气向东偏东气流形成的汇合线,以及主要由于汇合而引起的局部前缘形成,是这次暴雨的重要触发因素。大规模的强迫作用是主要的抬升机制,而潜在的额隆起在长三角北部的暴雨中起次要作用,而在南方的暴雨隆升的机制主要是局部的额下隆起引起大的CAPE释放,导致局部强浮力。隆起导致强烈的向上运动。双台风的汇聚不仅直接为暴雨提供了动态条件,而且通过加强高空和低空急流的耦合,二元台风也增强了动态升力。敏感性测试表明,长三角地区的暴雨对台风强度都敏感,而南部地区的降雨比北部地区的降雨更为敏感。基于上述因素,提出了二元台风条件下的长三角暴雨概念模型。 (C)2015 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《Atmospheric research》 |2015年第12期|33-48|共16页
  • 作者单位

    Zhejiang Inst Meteorol Sci, Hangzhou 310008, Zhejiang, Peoples R China|Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing 100081, Peoples R China;

    Zhejiang Inst Meteorol Sci, Hangzhou 310008, Zhejiang, Peoples R China;

    Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing 100081, Peoples R China;

    Coastal Carolina Univ, Sch Coastal & Marine Syst Sci, Conway, SC USA;

    Zhejiang Inst Meteorol Sci, Hangzhou 310008, Zhejiang, Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Binary typhoons; Rainstorm; Numerical simulation; Frontogenesis; Convergence line;

    机译:二元台风;暴雨;数值模拟;前生;会聚线;

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