一次典型雷暴事件的多普勒天气雷达观测与分析

B. Panda
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引用次数: 0

摘要

2018年4月25日,在印度奥里萨邦昌迪普尔地区附近探测到一场典型的衰减雷暴。这个逐渐减弱的雷暴最终产生了一股温暖的下沉气流,被称为热爆发。在短短10分钟内,环境温度上升了近5.3°C,相对湿度从81%降至22%。无线电探空数据显示,在海拔4公里处存在一个干层。由于地表逆温的存在和足够的下沉气流动量,下降的空气可以继续下降,超过其平衡水平到达地面。本文还深入研究了下沉气流对大气压力的影响。多普勒天气雷达(DWR)产品用于了解雷暴活动。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Observation and analysis of a typical thunderstorm event using Doppler Weather Radar products
A typical decaying thunderstorm was detected on 25th April 2018 in close proximity to Chandipur region of Odissa, India. This decaying thunderstorm ultimately produced a warm downdraft known as heat burst. Within a short span of 10 minutes, ambient temperature increased almost 5.3°C and relative humidity plunged from 81 % to 22%. Radiosonde data indicated the presence of a dry layer at an altitude of 4km. The presence of a surface based temperature inversion and with sufficient downdraft momentum, the descending air could continue downward beyond its equilibrium level to reach the surface. Effect of downdraft on atmospheric pressure has also been studied thoroughly. Doppler Weather Radar (DWR) products are used to understand the thunderstorm activities.
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