Partial Duration Trend Analysis for Yearly Rainfall and its Sequential Distribution: a Conceptual Model

R. Yadav, S. Saxena
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引用次数: 1

Abstract

In this study a new conceptual model for partial duration series analysis was applied to determine the likely rainfall of the monsoon season and the pattern of rainfall events distribution. Example case study was carried out with rainfall data of semiarid area, Agra, India, experiencing extremes of yearly rainfall; ranging between high (1200 mm) to low (300 mm). The coefficient values for the exponential decay function (K) were computed for all decays of partial dura- tion rainfall serises. Using the range of values of K and the yearly rainfall amounts further optimization produced the best results on the basis of the minimum Chi square value. The optimum K value was 0.92. Using this K, yearly rainfall values were predicted and compared with rainfall received for the validation period (1988-2002), not included in determination of optimum value of K. All the predicted yearly rainfall values were bit higher than observed ones. Further, for matching the predicted values with observed rain fall values, correction equations were also developed. For distribution of rainfall events in the year, successive rainfall event that could have preceded at any time were con- trasted with those of the past years with corresponding total rainfall values. As the rainy season progresses, the matching rainfall distribution of the corresponding rainfall year becomes the rainfall distribution pattern for year under the forecast; enabling selection of crops and cropping patterns before the onset of rainy season and carrying out strategic planning for successful agriculture under the changing scenario of rainfall pattern.
年降水量的部分历时趋势分析及其序列分布:一个概念模型
本文应用偏时序列分析的新概念模型来确定季风季节的可能降雨量和降雨事件的分布模式。以印度阿格拉半干旱区极端年降水数据为例进行了案例分析;范围从高(1200mm)到低(300mm)。对部分持续时间降雨序列的所有衰减计算指数衰减函数(K)的系数值。利用K值和年降雨量的范围进一步优化,在最小卡方值的基础上产生最佳结果。最佳K值为0.92。利用该K值对年降雨量进行了预测,并与验证期(1988-2002年)的降雨量进行了比较,而验证期(1988-2002年)的降雨量不包括在K的最优值的确定中。预测的年降雨量都略高于观测值。此外,为了使预测值与观测值相匹配,还建立了校正方程。对于年内降雨事件的分布,将可能在任何时间之前发生的连续降雨事件与过去具有相应总降雨量的年份进行对比。随着雨季的推进,相应降雨年的匹配降水分布成为预报下的年降水分布模式;在雨季来临前选择作物和种植模式,并在降雨模式变化的情况下为成功的农业开展战略规划。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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