Determination of precipitation return values in connection to severe rainfall event of 2010 in Pakistan

Z. Babar, Xiefei Zhi, Ling Zhang, F. Ge
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Abstract

Extreme weather events over Pakistan have been increasing. This is contributing to the ever enhancing human suffering of the region. The present study investigates the extreme rainfall in Pakistan by using General Pareto Distribution (GPD) method. This in turn is used to analyze extraordinary rainfalls of summer 2010. The results indicate that during the summer 2010 northwestern parts of Pakistan received abnormally high rainfalls. Of which a few places got rainfalls with return periods of more than fifty years. Mainly northern and north eastern parts of the country have the highest return year values during the monsoon season. Similarly south eastern parts of the country also show high return year values in summer. While most western parts of the country have small return year values in the monsoon or summer season. Climatologically these areas have comparatively less precipitation during summer monsoon. The weather pattern which developed in 2010 was not the usual convective weather system which is the hall mark of the monsoon season; instead it was a mesoscale convective system with stratiform precipitation.
2010年巴基斯坦强降雨事件降水回归值的确定
巴基斯坦的极端天气事件一直在增加。这助长了该区域不断加剧的人类苦难。本文采用一般帕累托分布(GPD)方法对巴基斯坦的极端降雨进行了研究。这反过来又被用来分析2010年夏季的异常降雨。结果表明,2010年夏季,巴基斯坦西北部地区降雨量异常高。其中一些地方的降雨周期超过50年。在季风季节,该国北部和东北部地区的年回报值最高。同样,该国东南部地区在夏季也显示出高回报年值。而该国大部分西部地区在季风或夏季的年回报值很小。在气候上,这些地区在夏季风期间降水相对较少。2010年形成的天气模式不是典型的季风季节的对流天气系统;相反,它是一个具有层状降水的中尺度对流系统。
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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