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The impact of electrified and non-electrified clouds on the inter-seasonal characteristics of surface based precipitation

机译:带电和不带电云对地表降水季节间特征的影响

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A multi-sensor analysis of the characteristics of electrified and non-electrified clouds along with their impact on the ground-based observation of raindrop size distribution (DSD) during the pre-monsoon and monsoon months of Indian Summer Monsoon over a heavy precipitation region of Western Ghat has been highlighted in the present paper. As the present region of study is instrumented with Ka-band Doppler Weather Radar, Microwave Radiometer and Joss-Waldvogel Disdrometer, hence an attempt has been made through this paper to address the result of investigation related to the characteristic pattern of clouds and precipitation associated with and without the lightning. The study initiated by analysing the morphology of vertical structure of clouds during various stages of a typical rainfall event which started initially with heavy precipitation, followed by lightning and finally ending with the precipitation accompanied by lightning. It was observed from the event that the initial heavy precipitation is basically due to the impact of the shallow convective cloud which is a natural phenomena of this region. The lightning is initiated in the presence of higher level clouds and finally when these higher level clouds joins the lower one, the precipitation accompanied with lightning begins.The impact of these modulations of clouds over the surface based DSD for the inter-seasonal rainfall events had also been portrayed through this study. The analysis reveals that during the pre-monsoon (monsoon) months, raindrops of larger diameter dominate the rainfall evolving from the non-electrified (electrified) clouds compared to the rainfall evolving from the electrified (non-electrified) ones. This is basically due to the convective nature of pre-monsoon rainfall where strong updraft lifts the smaller drops aloft and thereby allowing the larger drops to precipitate locally. As lightning is associated with higher level clouds, the raindrops evolving from them experiences more collision, coalescence and break-up procedure with respect to the rainfall evolving from low/middle level clouds before reaching the ground. Thus, larger drops are visible for rainfall evolving from non-electrified clouds during pre-monsoon season. While for the monsoon months, as most of the rainfall originates from the deep clouds, the chances of drops to break-up/evaporate is comparatively less for the precipitation evolving from electrified clouds with charged droplets in comparison to the non-electrified ones. Hence, drops of larger diameter dominate the monsoon rainfall associated with lightning.
机译:多传感器分析带电和不带电的云的特征,以及它们对印度洋季风在强降水区的季风前和季风月期间的雨滴大小分布(DSD)地面观测的影响。 Western Ghat在本文中已突出显示。由于目前的研究领域是用Ka波段多普勒天气雷达,微波辐射计和Joss-Waldvogel Disdrometer仪器进行的,因此,本文试图解决与云和降水相关的特征性模式有关的调查结果。并没有闪电。该研究通过分析典型降雨事件各个阶段中云的垂直结构形态而开始,该事件最初以强降水开始,然后是闪电,最后以降水伴随闪电结束。从该事件中观察到,最初的强降水基本上是由于浅对流云的影响,而浅对流云是该地区的自然现象。闪电是在高层云的存在下开始的,最终当这些高层云加入低层云时,伴随闪电的降水开始了。这些云调制对基于地面的DSD的季节间降雨事件的影响是这项研究也描述了这一点。分析表明,在季风前(季风)月份,与非电气化(非电气化)云降水相比,直径更大的雨滴主导了非电气化(电气化)云的降雨。这主要是由于季风前降雨的对流性质,强的上升气流将较小的液滴抬升到高处,从而使较大的液滴局部沉淀。由于闪电与较高级别的云有关,因此相对于低/中层云在到达地面之前所产生的降雨,从它们演变而来的雨滴经历了更多的碰撞,合并和分解过程。因此,对于在季风前季节非电气化的云所产生的降雨,可以看到更大的水滴。虽然在季风月份,由于大部分降雨来自深云,所以与不带电的液滴相比,带电液滴带电的云所产生的降水滴滴破裂/蒸发的机会相对较少。因此,直径较大的水滴主导着与闪电相关的季风降雨。

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