首页> 外文期刊>International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences >CHARACTERISTIC OF DROUGHT AND FLOOD IN THE DIAN-QIAN-GUI KARST AREAS BASED ON TRMM-Z INDEX
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CHARACTERISTIC OF DROUGHT AND FLOOD IN THE DIAN-QIAN-GUI KARST AREAS BASED ON TRMM-Z INDEX

机译:基于TRMM-Z指数的Dian-Qian-Gui岩溶地区干旱与洪水的特征

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In order to study the spatial and temporal variation of characteristics of drought and flood in Dian-Qian-Gui Karst Areas of China, TRMM 3B43 precipitation data from 1998 to 2017 and 72 rain gauge station data from 1998 to 2012 were used to verify the TRMM 3B43 data on monthly scale by correlation coefficient and relative deviation. The TRMM-Z index was taken as an index of drought and flood to quantitatively analyze the drought and flood characteristics. The results show that: (1) there was a significant positive correlation between TRMM 3B43 precipitation data and the measured data of meteorological stations on the monthly scale, with a correlation coefficient of 0.92, passing the significance test of 0.01 level. The calculated result of relative Bias is -0.058, indicating that TRMM 3B43 precipitation is slightly higher than the actual precipitation. (2) From 1998 to 2017, the TRMM-Z index in the research area fluctuated between −1.160 and 1.678, among which the Z index in July 1999 reached the maximum value of 1.678, and in February 2010 the Z index reached the minimum value of −1.160. (3) During the past 20 years, the flood months in the study areas were 47 months, accounting for 19.58% of the study time, and 40 months were drought months, accounting for 16.67% of the study time. Floods mainly occurred in the summer with abundant rainfall, while droughts mainly occurred in the winter with less rainfall. (4) Taking 2008–2009 as typical representative of drought and flood, the spatial variation of drought and flood were researched.
机译:为了研究中国滇桂王岩溶地区干旱和洪水特征的空间和时间变化,1998年至2017年的旱地3B43降水数据和1998年至2012年的雨量仪站数据从1998年到2012年验证了TRMM 3B43通过相关系数和相对偏差的每月规模数据。 TRMM-Z指数被视为干旱和洪水指数,以定量分析干旱和洪水特征。结果表明:(1)TRMM 3B43降水数据与月度规模的气象站测量数据之间存在显着的正相关性,相关系数为0.92,使其显着性试验为0.01级。相对偏置的计算结果为-0.058,表明TRMM 3B43沉淀略高于实际沉淀。 (2)从1998年到2017年,研究区的TRMM-Z指数波动在-1.160和1.678之间,其中1999年7月的Z指数达到了1.678的最大值,并于2010年2月达到最低价值-1.160。 (3)在过去的20年中,研究领域的洪水月为47个月,占研究时间的19.58%,40个月的干旱月份,占研究时间的16.67%。洪水主要发生在夏天,降雨充沛,而干旱主要发生在冬季,降雨量减少。 (4)采取2008 - 2009年典型的干旱和洪水的代表,研究了干旱和洪水的空间变化。

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