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Analysis of trends in rainfall and dry/wet years over a century in the Eastern Ganga Canal command

机译:在东部甘加运河东部趋势下降雨趋势及多年来干旱/潮湿阶段

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摘要

In the present study, an attempt has been made to analyse the variability and trends in annual and seasonal rainfall over the Eastern Ganga Canal command area, India. To determine the trend in annual/seasonal rainfall and rainy days, the non-parametric Mann-Kendall test and Sen's slope method were used over daily gridded rainfall for the time period 1901-2012. The results of the trend analysis revealed a decreasing trend in annual and monsoon rainfall in the range 18.5-61.7 and 19.4-56.7 mm/decade, respectively. For annual and monsoon rainy days, the results demonstrated a decreasing trend which varied from 1.8 to 2.9 and 1.4 to 2.2 days/decade, respectively, and an increasing trend in the range 0.2-1.4 and 1.0 days/decade, respectively. A variability analysis was performed to highlight the need for selecting an appropriate confidence level in trend analysis. It was observed that the grids showing a statistically non-significant trend at the 95% confidence level exhibit a statistically significant trend at lower confidence levels. An analysis of dry and wet years on an annual scale revealed that the chances of occurrence of a wet year are more in comparison with the chances of occurrence of a dry year in the command area by a ratio of 14:13. However, data from the last one and a half decades has a contradictory trend with higher chances of occurrence of a dry year to very minimal chances of occurrence of a wet year. Dependable rainfall at various probability levels was estimated using a gamma distribution function. It was observed that the 75% dependable weighted annual and seasonal rainfall over the command area (985.48 and 727.54 mm) was significantly different with respect to the climatic mean weighted annual and seasonal rainfall against the weighted mean annual and seasonal rainfall (1,165.93 and 901.95 mm).
机译:在本研究中,已经尝试分析了印度东部江卡渠道指挥区的年度和季节降雨中的变异性和趋势。为了确定年度/季节性降雨和雨天的趋势,非参数曼 - 肯德尔测试和森坡度的斜坡法在1901-2012时期的日常喷射降雨量上使用。趋势分析的结果揭示了18.5-61.7和19.4-56.7毫米/十年的年度和季风降雨量的降低。对于年度和季风雨天,结果表明,分别从1.8〜2.9和2.2天/十年变化的降低趋势,分别增加了0.2-1.4和1.0天/十年的趋势。进行了可变性分析以突出趋势分析中选择适当的置信水平的需要。据观察,在95%置信水平上显示出统计上非重大趋势的网格在较低的置信水平下表现出统计上显着的趋势。对年度规模的干燥和潮湿年份的分析表明,与指挥面积的干燥年的发生机会,潮湿年的发生的可能性更为比较14:13。然而,来自最后一十年和半年的数据具有矛盾的趋势,可能发生了较高的潮湿年度的最低机会的干燥年度。使用伽马分布函数估计各种概率水平的可靠降雨。据指出,在指挥范围(985.48和727.54 mm)上的75%可靠的加权年和季节降雨与加权平均年和季节降雨量的气候平均加权年度和季节降雨(1,165.93和901.95 mm)显着不同)。

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