一次台风暴雨过程的诊断分析
Diagnostic Analysis of a Typhoon and Rain Process
DOI: 10.12677/CCRL.2019.86080, PDF,   
作者: 杨 萌*, 王文波, 王世杰:山东省潍坊市气象局,山东 潍坊
关键词: 台风高空急流副热带高压冷空气Typhoon Upper Level Jet Subtropical High Cold Air
摘要: 本文利用MICAPS常规观测资料对2014年7月24日~25日影响山东的台风“麦德姆”进行研究,着重分析其路径、形成暴雨的成因和物理量等。研究表明本次过程是一次北上台风影响山东的过程。强大副高的阻挡是本次过程的特殊环流形势,使得台风一直保持较高的偏北分量,为本次暴雨形成提供了有利条件。台风沿副高外围引导气流先向北后向东北方向移动,在鲁中东部和半岛降水条件非常有利,此次降水主要发生在台风中心附近和东北象限区域内,台风外围云系与冷空气相互作用可能造成短时强降水。
Abstract: In this paper, the MICAPS conventional observation data is used to study the typhoon "Matmo" which affects Shandong from July 24th to 25th, 2014, focusing on the analysis of its path and the causes and physical quantities of heavy rain. Studies have shown that this process is a process of typhoon north affecting Shandong. The blockage of the strong sub-high is the special circulation situation of this process, which makes the typhoon always maintain a high northerly component, which provides favorable conditions for the formation of heavy rain. The typhoon moves along the periphery of the subtropical high to move northward and backward to the northeast. The precipitation conditions in the eastern part of Shandong Province and the peninsula are very favorable. The precipitation mainly occurs in the vicinity of the typhoon center and the northeast quadrant. The typhoon’s peripheral cloud system and the cold air interact with each other. The effect may be caused by short-term heavy precipitation.
文章引用:杨萌, 王文波, 王世杰. 一次台风暴雨过程的诊断分析[J]. 气候变化研究快报, 2019, 8(6): 739-748. https://doi.org/10.12677/CCRL.2019.86080

参考文献

[1] 郭荣芬, 鲁亚斌, 李燕, 等. “伊布都”台风影响云南的暴雨过程分析[J]. 高原气象, 2005, 24(5): 784-791.
[2] 姚才. 0103号台风“榴莲”强度变化特征及暴雨成因的分析[J]. 热带气象学报, 2003, 19(增刊): 180-188.
[3] 杨宇红, 沈新勇, 林两位, 等. 0418号台风艾莉暴雨成因分析[J]. 气象, 2006, 32(7): 81-87.
[4] 何立富, 尹洁, 陈涛, 等. 0509号台风麦莎的结构与外围暴雨分布特征[J]. 气象, 2006, 32(3): 93-100.
[5] 余贞寿, 高守亭, 任鸿翔. 台风“海棠”特大暴雨数值模拟研究[J]. 气象学报, 2007, 65(6): 864-876.
[6] 魏建苏, 赵永玲, 等. “0012”台风引发“8.30”特大暴雨过程的分析[J]. 气象科学, 2003, 23(1): 92-99.
[7] 孙建华, 齐琳琳, 赵思雄. “9608”号台风登陆北上引发北方特大暴雨的中尺度对流系统研究[J]. 气象学报, 2006, 64(1): 57-71.
[8] 李兆祥, 杨克明. 黄淮气旋及其预报[J]. 气象, 1980, 6(4): 1-4.
[9] 黄彬, 代刊, 钱奇峰, 等. 引发黄渤海大风的黄淮气旋诊断研究[J]. 气象, 2013, 39(4): 302-312.
[10] 苗春生, 宋萍, 王坚红, 等. 春夏季节黄淮气旋经渤海发展时影响因子对比研究[J]. 气象, 2015, 41(9): 1068-1078.
[11] Uccellini, L.W., Keyse, D., Brill, K.F., et al. (1985) Wash the President’s Day Cyclone of 18-19 February 1979: Influence of Upstream Trough Amplification and Associated Tropopause Folding on Rapid Cyclogenesis. Monthly Weather Review, 113, 962-988. [Google Scholar] [CrossRef
[12] 丁治英, 王劲松, 翟兆锋. 爆发性气旋的合成诊断及形成机制研究[J]. 应用气象学报, 2001, 12(1): 30-40.