摘要
用青藏高原５个站从１９５６～１９８６年共３１年的０．８ｍ地温距平，计算了秋季（９～１１月）的地温异常，同时考虑了我国汛期（４～９月）及夏季（６～８月）的降水相关，发现两者相关很好。不同部位的高原地温异常对我国降水关系的区域是不相同的。本文为中国汛期降水预报提供了依据。
The ground temperature departure of Qinghai-Xizang Plateau at0．8m level in autumn is calculated by means of 5 stations. A nice correlation between the precipitation of flood seasons and that of summer seasons is discovered．The ground temperature deportures in different regions of the plateau have different influence on the precipitation in China. This provides a foundation for precipitation forcast of flodseasons in China.
基金
国家基础性研究重大关键项目"气候动力学和气候预测理论的研究"资助
关键词
青藏高原
地温异常
汛期
降水
相关
中国
：Qinghai-Xizang Plateau；Ground temperature departure；Precipitation of flood seasons； Correlation.
