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Assessment of Trends and Variability of Rainfall and Temperature for the District of Mandi in Himachal Pradesh, India

机译:印度喜马al尔邦曼迪地区降雨量和温度的趋势和变异性评估

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Climate variability, particularly, that of the annual air temperature and precipitation, has received a great deal of attention worldwide. The magnitude of the variability of the factors changes according to the locations. The present study focuses on detecting the trends and variability in the annual temperature and rainfall for the district of Mandi in Himachal Pradesh, India. This study used annual and monsoon time series data for the time period 1981-2010 and modified the Mann-Kendall test and Sen's slope estimator in analyzing the problem. The results of the analysis indicate that the annual maximum temperature (TMX) and annual minimum temperature (TMN) for the period of 30 years have shown an increasing trend, whereas the monsoon’s maximum and minimum temperatures have shown a decreasing trend, although it is statistically not significant. The amount of annual rainfall does not show any significant trend, but the monsoonal rainfall has shown an increasing trend that is also statistically not significant. The resulting Mann-Kendall test statistic (Z) and Sen’s slope estimate (Q) of all the parameters studied indicate that changes are occurring in the magnitude and timing of the precipitation and temperature events at the Mandi station.
机译:气候变化,特别是年度气温和降水的气候变化,已引起全世界的广泛关注。这些因素的可变性的大小根据位置而变化。本研究的重点是检测印度喜马al尔邦曼迪地区年温度和降雨量的趋势和变化。这项研究使用了1981-2010年期间的年度和季风时间序列数据,并对Mann-Kendall检验和Sen的斜率估计器进行了分析。分析结果表明,尽管在统计上是统计的,但30年期间的年最高温度(TMX)和年最低温度(TMN)呈上升趋势,而季风的最高和最低温度呈下降趋势。不重要。年降水量没有显示任何明显的趋势,但季风性降水却显示出增加的趋势,在统计上也并不显着。得到的所有参数的Mann-Kendall测试统计量(Z)和Sen的斜率估计值(Q)表明,Mandi站降水和温度事件的大小和时间发生了变化。

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