翟羽佳, 周常春, 刘春学. 苍山十八溪流域近60年降水量时空分布特征分析[J]. 云南大学学报(自然科学版), 2017, 39(4): 618-623. doi: 10.7540/j.ynu.20160550
引用本文: 翟羽佳, 周常春, 刘春学. 苍山十八溪流域近60年降水量时空分布特征分析[J]. 云南大学学报(自然科学版), 2017, 39(4): 618-623. doi: 10.7540/j.ynu.20160550
ZHAI Yu-jia, ZHOU Chang-chun, LIU Chun-xue. An analysis on the spatial and temporal distribution of precipitation of eighteen creeks' watershed in Cangshan Mountain[J]. Journal of Yunnan University: Natural Sciences Edition, 2017, 39(4): 618-623. DOI: 10.7540/j.ynu.20160550
Citation: ZHAI Yu-jia, ZHOU Chang-chun, LIU Chun-xue. An analysis on the spatial and temporal distribution of precipitation of eighteen creeks' watershed in Cangshan Mountain[J]. Journal of Yunnan University: Natural Sciences Edition, 2017, 39(4): 618-623. DOI: 10.7540/j.ynu.20160550

苍山十八溪流域近60年降水量时空分布特征分析

An analysis on the spatial and temporal distribution of precipitation of eighteen creeks' watershed in Cangshan Mountain

  • 摘要: 依据苍山十八溪流域4个气象观测点近60年来(1951—2013年)逐月的降水量观测资料,运用地质统计学中变异函数的相关理论和方法,分析了十八溪流域降水量的时空分布规律.结果表明:在时间上,流域平均降水量呈周期性变化,总趋势在减少,2009年以后进入新的少雨期,流域月平均降水量丰沛的季节主要集中在5—10月,稀少的季节主要集中在11—4月,干湿分明;在空间上,流域降水主要分布在流域中部靠近洱海的地区以及苍山东面的狭长地区,呈现东西地区年降水量差异悬殊的趋势.

     

    Abstract: This paper applied the variogram of geostatistics to analyze the spatial and temporal distribution of the Cangshan eighteen creek precipitation using time series of Dali meteorological stations' data of monthly mean precipitation from 1951—2013.The results showed that there existed two main oscillation cycle patterns with different timescales in monthly mean precipitation and the precipitation of the studied area was reduced annually,and entered a new low rainfall period after 2009.The season of rainfall was mainly concentrated from May to October,and the sparse season was mainly concentrated from November to April in next year.The spatial distribution of monthly precipitation showed the characteristics of the obvious regional gap.The region of abundant rainfall concentrated in the central valley near the Erhai and the narrow area in the east of Cangshan.

     

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