Impact of Typhoons of Different Intensities on Short-Term Precipitation in the Middle and Lower Reaches of the Yangtze River in Summer

IF 2.1 4区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES
Zhongwu Zhang
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引用次数: 1

Abstract

According to China’s reanalyzed meteorological dataset (CN05.1), a 6-h track intensity typhoon meteorological dataset in the Western Pacific, three types of short-term precipitation are described to study the impact of typhoons on summer rainfall of different intensities in the middle and lower reaches of the Yangtze River: short-term extreme precipitation (95% quantile), short-term heavy precipitation (75% quantile), and normal precipitation (below the lower limit of the 75% quantile threshold). The results show that the amount of short-term extreme precipitation is 1.8 and 3.7 times that of normal precipitation and short-term heavy precipitation, respectively. Considerable interannual and interdecadal fluctuations in the proportion of short-term heavy precipitation and extreme precipitation during summer are affected by typhoons, with a wide range of changes occurring between 1980 and 2000. The areas with high amounts of short-term heavy precipitation and extreme precipitation are distributed mostly in the middle and southern parts of the middle and lower reaches of the Yangtze River, whereas areas with a high amount of normal precipitation are distributed mostly in the southeastern parts of the river. The spatial distribution of the three intensities of rainfall affected by typhoons is consistent, with a gradual decrease from southeast to northwest; in addition, the spatial distribution of the proportion of total summer rainfall has similar characteristics. The three intensities of precipitation are affected by the spatial distribution of the typhoon path frequency, and the distribution of the high-value areas is essentially the same as that of precipitation. This indicates that most of the typhoons that affect summer precipitation pass through the middle and lower reaches of the Yangtze River.
不同强度台风对长江中下游夏季短时降水的影响
根据中国西太平洋6小时路径强度台风气象数据集(CN05.1),描述了三种类型的短期降水,研究了台风对长江中下游不同强度夏季降水的影响:短期极端降水(95%分位数),短期强降水(75%分位数)和正常降水(低于75%分位数阈值的下限)。结果表明,短时极端降水量分别是正常降水量和短时强降水量的1.8倍和3.7倍。夏季短期强降水和极端降水比例的年际和年代际波动很大,受台风影响,1980年至2000年期间变化范围很大。短时强降水量和极端降水量高的地区主要分布在长江中下游中南部,正常降水量大的地区多分布在长江东南部。台风影响的三种降雨强度的空间分布是一致的,从东南到西北逐渐减弱;此外,夏季总降水量占比的空间分布也具有相似的特征。三种降水强度受台风路径频率空间分布的影响,高值区的分布与降水基本相同。这表明,影响夏季降水的台风大多经过长江中下游地区。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Advances in Meteorology
Advances in Meteorology 地学天文-气象与大气科学
CiteScore
5.30
自引率
3.40%
发文量
80
审稿时长
>12 weeks
期刊介绍: Advances in Meteorology is a peer-reviewed, Open Access journal that publishes original research articles as well as review articles in all areas of meteorology and climatology. Topics covered include, but are not limited to, forecasting techniques and applications, meteorological modeling, data analysis, atmospheric chemistry and physics, climate change, satellite meteorology, marine meteorology, and forest meteorology.
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