摘要
应用T检验方法对我国黄河中游地区1470~1991年夏季(5~9月)旱涝等级序列进行分析,结果表明:该地区气候存在着两次百年尺度突变,即17世纪50年代前后(早转涝)和18世纪60年代初期(涝转正常),以及百年尺度内20~30年尺度的气候突变;并指出黄河中游地区各时期旱涝变化与赤道东太平洋海温指数(SSTI)和大气活动中心的演变有密切联系.
The summer dryness/wetness grades series for the last 522 years (1470-1991 ) in the middle reaches of Yellow River are analysed by T test. The results indicate that there are two abrupt changes with 100-year scale in this region, around 1650's (from drought to flood) and in the early 1760' s(from flood to normal). There are also jumps of 20~30 year scale within the 100-year scale variations. It is also found that the drought/flood in the region are associated with the evolution of atmospheric active centers and the Sea Surface Temperature Index (SSTI) of the equatorial East Pacific.
出处
《应用气象学报》
CSCD
北大核心
1996年第1期89-95,共7页
Journal of Applied Meteorological Science
基金
国家重点课题
长期预报课题
关键词
黄河
中游地区
海温
大气活动中心
旱涝
The middle reaches of Yellow River
Abrupt change of climate
Sea surface temperature
Atmospheric active centre