水文
水文
수문
HYDROLOGY
2009年
5期
82-85
,共4页
次洪%雨强%气候变化%人类活动%孤山川
次洪%雨彊%氣候變化%人類活動%孤山川
차홍%우강%기후변화%인류활동%고산천
flood%rainfall intensity%climate change%human activity%Gushanchuan
利用有序聚类法、MWP检定法分析出1979年为孤山川流域天然时期和人类活动影响时期水沙的转折点,采用1979年之前的资料建立模型,并将该时期的次洪水量和沙量作为基准,分析了气候变化和人类活动对1979年后次洪水量和沙量的影响.
利用有序聚類法、MWP檢定法分析齣1979年為孤山川流域天然時期和人類活動影響時期水沙的轉摺點,採用1979年之前的資料建立模型,併將該時期的次洪水量和沙量作為基準,分析瞭氣候變化和人類活動對1979年後次洪水量和沙量的影響.
이용유서취류법、MWP검정법분석출1979년위고산천류역천연시기화인류활동영향시기수사적전절점,채용1979년지전적자료건립모형,병장해시기적차홍수량화사량작위기준,분석료기후변화화인류활동대1979년후차홍수량화사량적영향.
The turning point of water and sand of natural period and human activities impact period in Gushanchuan Basin is the year 1979,which was analyzed with the method of orderly clustering and MWP test.The model was established with the data before 1979.and the runoff and sediment transportation during this period was regarded as benchmark value.The impacts of climate change and human activities on the quantity of water and sediment during floods after 1979 were analyzed.
