摘要
分析、研究华北和邻近的辽宁地区曾发生过的“58.7”、“63.8”、“75.8”和“30.8”等4次罕见特大暴雨,结果表明,它们的气象学成因都是由于热带、副热带、西风带三种不同性质的天气系统的特定配置,引起暖湿气流和干冷气流在本区交绥所致。而这些天气系统的特定配置又与引潮力共振的特定迭加有密切联系。尤其是在暴雨天气形势具备之后,如果华北继续遇引潮力共振减压的迭加,将触发罕见特大暴雨的发生。其中台风在影响本区时(假定台风登陆我国大陆时强度为35m/s),如遇一个引潮力共振减压,当天的最大日降水可达500mm左右;如一天内遇两个引潮力共振减压的迭加,则当天的最大日降水将达1000mm左右。
Four exceptionally serious rainstorm events occured in North China and Liaoning Province, namely the '58.7','63.8','75.8' and '30.8' rains. With a review of their meteorological background and possible causes, this paper points out that the specific disposition of three different synoptic systems of tropical, subtropical and westerly belts causes the meeting of the air current of warm-wet and cold-dry in this area, and this kind of disPOsition of the synoptic systems is closely related to the specific superposition of tide-forming force resonance. Especially, if the rainstorm synoptic situation dominates in North China, with a continuously meeting of the superposition of pressure decrease of tide-forming force resonance, it can tfigger off an exceptionally serious rainstorm. Concret6iy, when a typhoon affects this area (assuming that the typhoon nit6nsity is 35m/s at landing the Chinese Continent), the daily maximum rainfall could reached about 500mm if the pressure decrease of one tideforming force resonance occures, and the daily maximum rainfall could reached about 1,000 mm if the superposition of pressure decrease of tWo tide-forming force resonance occures during the period of a day.
出处
《水科学进展》
EI
CAS
CSCD
1994年第4期255-261,共7页
Advances in Water Science
关键词
特大暴雨
天气系统
引潮力共振
形成
华北地区
serious rainstorm
tide-forming force resonance
tropical belt
subtropical
westerly belt
meeting of synoptic systems