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Spatial and temporal analysis of thunderstorm and rainfall activity over India

机译:印度雷暴和降雨活动的空间与时间分析

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Thunderstorms are one of the most devastating mesoscale severe weather phenomena, which play an important role in the occurrence of rainfall activity over a region. Therefore, in the present study an attempt has been made to identify the relationship between thunderstorm days (Thn), rainy days (Thr) and rainfall amounts (Trr) for 294 meteorological stations spreading over India, by means of published data (climatological normals) from the India Meteorological Department (IMD) for four periods, 1951-1980, 1961-1990, 1971-2000, and 1981-2010. The analysis has revealed a sharp decrease in the frequency of Thn, while Thr and Trr showed a slight decline. A significant correlation between Thn, Thr and Trr has been observed. Monthly analysis has exhibited a dual peak in the occurrence of Thn and single peak in rainfall activity; however, a time lag of one month in their peak occurrence was detected. These results show that the Indian summer monsoon affects significantly the thunderstorm activity over India. Seasonal analysis suggests that Thn, Thr and Trr are maximum during the monsoon season, while minimum during winters. Apart from this, Thn and Thr. and Thn and Trr have demonstrated a negative relationship during the monsoon, which may be anomalously due to decreasing temperature in India during that season. In addition, the spatial annual and seasonal pattern of the occurrence of Thn, Thr and Trr shows almost a similar pattern during 1951-1980. However, a sharp decline in the frequency of Thn has been observed during subsequent periods over all parts of the country. Likewise, a slight decline in the frequency of Thr and Trr has been observed over India, except in the northeast, where an increasing trend in rainfall activity has been observed. The computed ratio between Thn and Thr (R) has been found maximum during the pre-monsoon, whereas the ratio between Trr and Thn (RTR) during the monsoon season. Regional analysis of Thn, Thr and Trr revealed a wide range of variations in the occurrence of these parameters month after month. It is believed that the results presented in this study will be useful for weather forecasters, aircraft pilots, agriculturists and planners.
机译:雷暴是最具破坏性的迈空硕士恶劣天气现象之一,在该地区的降雨活动发生时发挥着重要作用。因此,在本研究中,通过发表的数据(气候法线),已经尝试识别雷暴天(THN),雨天日(THN),下雨天(THR)和降雨量(TRR)之间的关系(TRR)。来自印度气象部门(IMD)四期,1951-1980,1961-1990,1971-2000和1981-2010。分析显示THN频率的急剧下降,而THR和TRR显示出轻微的下降。已经观察到THN,THR和TRR之间的显着相关性。每月分析在降雨量活动中出现了双峰和单峰峰;然而,检测到在其峰值发生中一个月的时间滞后。这些结果表明,印度夏季季风对印度的雷暴活动大大影响。季节性分析表明,在季风季节,THN,THR和TRR最大,而冬季期间最少。除此之外,thn和thr。并且THN和TRR已经展示了季风期间的负面关系,这可能是由于在该季节期间印度的温度降低而受到严重的。此外,在1951年至1980年期间,THN,THR和TRR发生的空间年度和季节性模式几乎是一种类似的模式。然而,在随后在该国所有地区的后期观察到THN频率的急剧下降。同样地,在印度除了在东北部之外观察到Thr和TRR频率的略微下降,除了在东北部门,已经观察到降雨活动的越来越大的趋势。在季风前,THn和Thr(R)之间的计算比率最大,而TRR和THN(RTR)之间的比率在季风季节。 THN,TROR和TRR的区域分析显示了这些参数在月份之后发生的广泛变化。据信,本研究中提出的结果将对天气预报员,飞机飞行员,农业学家和规划者有用。

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