摘要
通过对近百年来黄河流域各区域旱涝气候突变特征的研究,表明该流域的大部分地区旱涝气候变化在本世纪10年代内出现突变现象,而且是从一个相对的偏涝期进入偏早期的转变。并且初步分析了黄河流域出现旱涝气候突变的可能成因。
In this paper,the drought/flood indexes for the divisions in the Huanghe River Basin during the last 100 years (1891—1990) are analysed to reveal abrupt climatic change using the Mann-Kendall Test.It is found that there existed abrupt climatic change of drought/flood in 1910 and 1912 over the middle and lower reaches respective- ly,but no such obvious abrupt climatic change is found over the upper reaches.These facts show that there existed abrupt climatic changes of drought/flood for most parts of the basin during the 1910s,which were jumps from flood to drought phases.Meanwhile, it is should be pointed out that the jump was not non-local event in the basin.In addi- tion,the possible reasons causing the jumps are discussed.By analysing the South Oscil- lation Index and the air temperature of the Northern Hemisphere using the same test, one can see that their abrupt changes occurred earlier than that of the drought/flood,in- dicating that these may be improtant background conditions for the event of abrupt cli- matic change of drought/flood.
出处
《地理科学》
CSSCI
CSCD
北大核心
1993年第4期315-321,共7页
Scientia Geographica Sinica
关键词
旱涝
气候
气候变化
黄河流域
Drought/flood
Abrupt climatic change
Southern Oscillation