文章摘要
裴生山,张顺桂,张思芳,许德基.青海湖流域降水量变化趋势分析Journal of Water Resources and Water Engineering[J].,2013,24(4):217-219,224
青海湖流域降水量变化趋势分析
Analysis of change trend of precipitation in Qinghai Lake basin
Received:January 10, 2013  Revised:February 27, 2013
DOI:
中文关键词: 降水量  变化趋势  青海湖
英文关键词: precipitation  change trend  Qinghai Lake
基金项目:
Author NameAffiliation
PEI Shengshan Hydrology Water Resources Survey Bureau of Qinghai Province, Xining 810000,China 
ZHANG Shungui Qinghai Province Land EC Levy Center, Xining 810008,China 
ZHANG Sifang Huangzhongxian Municipal Bureau of Qinghai Province,Huangzhong 811600,China [KH*5D] 
XU Deji Hydrology Water Resources Survey Bureau of Qinghai Province, Xining 810000,China 
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中文摘要:
      降水是地球上陆地各种水体的直接或间接补给源。根据青海湖流域降水量资料采用Kendall秩次检验、Spearman秩次检验及线性趋势回归检验3种方法对流域内降水量变化趋势进行了分析计算,得出了降水量增加趋势比较明显的结论,说明青海湖水位近十几年下降趋势变缓是由于降水量的增加引起的。研究结果为该流域降水和水资源预测提供参考。
英文摘要:
      Precipitation is the direct or indirect supply source of various water body in land. According to Qinghai lake basin precipitation data and using the three methods of Kendall rank time, Spearman rank time and linear trend regression test ,the paper calculated and analyzed the variation trend of precipitation in the basin ,and got the conclusion that the increase trend of precipitation is obvious, the decline of water level in Qinghai lake for ten years become slow because of the increase of precipitation. The result can provide reference for the prediction basin rainfall and water resources.
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