摘要
利用1951—2001年10月～4月台湾及中蒙西部强地震资料,研究了它与中国大陆降水场的关系。结果表明:台湾冬春季强震之后的夏季长江及江南不会多雨;冬春季台湾及中蒙西部(70°～103°E)同时有≥6.9级强震出现时,我国长江以北会有一块地区出现洪水。
Based on the data of precipitation and earthquake from 1951 to 2001, the relationship between summer precipitation in mainland and the destructive earthquake in Taiwan and western ChinaMongolia are analyzed. The conclusion obtained are as follows: When the destructive earthquakes occurred during last year(October to next April), the Yangtze River and Jiangnan area will not be wet (less precipitation)in this year summer. When the destructive earthquakes(≥6.9) occurred both in Taiwan and western ChinaMongolia, a flood area will be appeared over the regions north to the Yangtze River.
出处
《高原气象》
CSCD
北大核心
2003年第6期643-645,共3页
Plateau Meteorology
基金
国家重点基础研究发展规划项目(G1998040800)资助
关键词
台湾强震
中蒙西部强震
夏季降水
Taiwan, western China-Mongolia destructive earthquakes
Summer rainfall
