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《Scientia Geographica Sinica》 2009-04
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Changes of Seasonal Precipitation of Yuanmou Dry-hot Valley in Recent 50 Years Based on method of DFA

ZHANG Bin1,SHI Kai2,LIU Chun-qiong2,AI Nan-shan3,LIU Gang-cai4,QIN Fa-chao1(1.Land and Resources College,China West Normal University,Nanchong,Sichuan 637009;2.School of Biological Resources and Environmental Sciences,Jishou University,Jishou,Hunan 416000;3.School of Architecture and Environment,Sichuan University,Chengdu,Sichuan 610065;4.Institute of Mountain Harads and Environment,Chinese Academy of Sciences,Chengdu,Sichuan 610041)  
The dry-hot valley is a special kind of ecosystem degradation region in Hengduan Mountains.Changes of seasonal precipitation have important influnces on its landscape patterns and agricultural activities.Based on the method of Detrended Fluctuation Analysis(DFA),the trend of seasonal precipitation of Yuanmou Dry-hot Valley during 1956-2006 and moving series during 1978-2006 are anlyzed.The results show that there is an obvious Hurst Effect at scale of 50 years as to the time series of seasonal precipitation of Yuanmou Dry-hot Valley—relative weak persistent long-range and relative strong randomness in the summer and winter,relative weak anti-correlation in the spring and autumn.Change of underlying surfaces,caused by the annual and seasonal changes of biomass and vegetation coverage,is contributed to the seasonal variations of precipitation.
【Fund】: 国家支撑计划项目(2006BAC01A11);; 国家重点基础研究发展计划(973)项目(2007CB407206)资助
【CateGory Index】: P468.024
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