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黄河中游地区近522年旱涝突变
引用本文:于淑秋,林学椿.黄河中游地区近522年旱涝突变[J].应用气象学报,1996,7(1):89-95.
作者姓名:于淑秋  林学椿
作者单位:1.中国气象科学研究院
基金项目:国家重点课题,长期预报课题
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(旱转涝)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。

关 键 词:黄河中游地区    气候突变    海温    大气活动中心

Abrupt Change of Drorght/Flood for the Last 522 Years in the Middle Reaches of Yellow River
Yu Shuqiu,Lin Xuechun.Abrupt Change of Drorght/Flood for the Last 522 Years in the Middle Reaches of Yellow River[J].Quarterly Journal of Applied Meteorology,1996,7(1):89-95.
Authors:Yu Shuqiu  Lin Xuechun
Institution:1.(Chinese Academy of Meteorological Sciences, Beijing 100081)
Abstract: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.
Keywords:The middle reaches of Yellow River  Abrupt change of climate  Sea surface temperature  Atmospheric active centre
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