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The characteristic of short-duration heavy rain under the 500 hPa subtropical high of west Pacific in autumn 2010 and the application of mesoscale weather chart analysis

机译:2010年秋季西太平洋500 hPa亚热带高压下的短时暴雨特征及中尺度天气图分析的应用

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By using the synoptic chart, densified observation of precipitation and sounding data, the characteristic of the short-duration heavy rain which occurred over China mainland under the region which controlled by 500 hPa Subtropical High of west Pacific in autumn 2010 are analyzed. Moreover, the typical examples are analyzed by mesoscale weather chart anaysis. Then the respect of mesoscale weather chart analysis would be given. Results demonstrate that the short-duration heavy rain is familiar in the region which controlled by 500 hPa Subtropical High of west Pacific in autumn 2010, especially in September. The occurrence days of short-duration heavy rain in the region which controlled by 500 hPa Subtropical High of west Pacific in autumn 2010 are decreased from September to Aoctober. The occurrence days of short-duration heavy rain in September are the most which are 76.7% of the Subtropical high control days. In autumn the occurrence days of Short-duration heavy rain which controlled by Subtropical High are 47.5% of the Subtropical high control days. The short-duration heavy rain under the region which controlled by subtropical high occur in the forenoon more than in the afternoon except in November. In November there is no short-duration heavy rain under the region which controlled by 500 hPa subtropical high of west Pacific. When we analyze the short-duration heavy rain under the 500 hPa subtropical high of west Pacific in autumn 2010 by using the mesoscale weather chart analysis, we should pay attention to the significant moist region in the low level, the baroclinicity of Subtropical High, convergence of air flow in the low level, orographic uplift, 925 hPa level, thermal condition of surface and convergence of water vapour etc..
机译:利用天气图,降水和测深资料的密实观测,分析了2010年秋季在西太平洋500hPa亚热带高压控制下的中国大陆上发生的短时暴雨的特征。此外,通过中尺度天气图分析对典型实例进行了分析。然后,将对中尺度天气图分析给予重视。结果表明,在2010年秋季,特别是9月,在受西太平洋500 hPa亚热带高压控制的地区,短时暴雨是熟悉的。在2010年秋季,受西太平洋500 hPa亚热带高压控制的地区,短时暴雨的发生天数从9月减少至10月。 9月,短时暴雨的发生天数最多,为亚热带高控天数的76.7%。在秋季,受副热带高压控制的短时暴雨发生天数是副热带高压控制天数的47.5%。在副热带高压控制下的地区,短时暴雨发生在前夕,比11月除外,下午更多。在11月,西太平洋500hPa亚热带高压控制下的区域没有短时大暴雨。当使用中尺度天气图分析对2010年秋季西太平洋500hPa亚热带高压下的短期暴雨进行分析时,应注意低层的显着湿润地区,亚热带高压的斜压性,收敛性。低空气流,地形隆起,925 hPa水平,地表热状况和水蒸气汇聚等。

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