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Some Features of Surface Air Temperature: A Statistical Viewpoint

机译:地表气温的一些特征:统计观点

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A climatological study has been done in five weather stations viz Dhuburi, Guwahati, Silchar, Tezpur and Dibrugarh for 45 years (1969-2013), for studying and comparing maximum, minimum and mean temperatures. Coefficient of variation, skewness, kurtosis are also calculated and plotted for comparing the results of the stations. The values of period mean of annual surface air temperature are different at different stations and this value does not show homogeneous distribution in the regions. The pattern of distribution of annual mean of daily surface air temperature (maximum, minimum and mean) are asymmetrical over all the stations and have different peakedness at different stations means over all the stations that the distribution are deviates from the normal distribution from slight to significant amount. In most of the cases winter months has shown highest variation while summer month are least variable. Variation in spring and autumn months are in between these two extremes. Almost over all the stations, the patterns of distribution of monthly mean temperature (maximum, minimum and mean) are not normal. The distributions are both positively and negatively skewed and have both platykurtic and leptokurtic peakedness.
机译:为了研究和比较最高,最低和平均温度,已在五个气象站进行了气候学研究,即Dhuburi,Guwahati,Silchar,Tezpur和Dibrugarh,长达45年(1969-2013年)。还计算出变异系数,偏度,峰度,并作图以比较测站结果。在不同的站点上,年度地面空气温度的周期平均值的值是不同的,并且该值在区域中没有显示出均匀的分布。在所有站点上,每日地面空气温度的年平均分布(最大值,最小值和平均值)的分布方式是不对称的,并且在不同站点上具有不同的峰值,这意味着在所有站点上,其分布均从正态分布(从轻微到显着)偏离量。在大多数情况下,冬季月份变化最大,而夏季月份变化最小。春季和秋季月份的变化介于这两个极端之间。几乎在所有测站上,月平均温度(最高,最低和均值)的分布方式都不正常。分布既有正偏也有负偏,并且具有峰峰值和峰峰值。

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