利用雷达产品和himawai -8气象卫星解译识别Puting - belung事件(以2018年11月22日雅加达Puting - belung事件为例)

I. Rusmala
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引用次数: 0

摘要

2018年11月22日,印度尼西亚雅加达地区再次发生类似“普廷”或龙卷风的事件。这一事件造成了许多损失。在此基础上,研究了用反射率产品来识别钩回波和弓形回波型,用速度产品来识别中气旋型,作为普亭北斗雷达产品的特点。本研究使用的曾卡伦c波段原始数据雷达,经HWIND处理得到0.5 km、1.0 km和1.5 km高程的CMAX、VCUT和CAPPI (V)叠加。利用CMAX和VCUT雷达产品,通过观测产生普亭贝隆的云的最高反射率,确定了引起普亭贝隆的云结构。然后利用HWIND的CAPPI产品叠加来识别该风的运动,该风的运动被怀疑是在该位置形成一个以风分量和径向速度形式存在的中气旋型为特征的普亭束的开始。有人怀疑雅加达中部地区有风在旋转,这表明该地区有普亭旋风。然后,利用卫星图像检测形成普亭洞的积雨云,验证了雷达解释的分析。根据这项研究,我们知道普亭事件发生在世界时08.12左右。产生气旋的云增长迅速,反射率在35 ~ 45 dBZ之间,风速可达35节。卫星图像分析显示,云峰温度明显下降,以积雨云形式形成的对流云表明了普亭流现象。然而,在这个案例中,从旋转径向速度分量的中气旋型中可以看出普亭-贝林现象,而不是从钩回波或弓形回波型中可以看出。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Identification of the Puting Beliung Event by Utilizing the Interpretations of Radar Products and Himawari-8 Weather Satellite (Case Study: Puting Beliung Incident, November 22, 2018 in Jakarta)
Indonesia was shocked again by a Puting beliung or tornado-like incident on November 22, 2018, in the Jakarta area. This incident caused many losses. In this regard, a study was conducted to observe the reflectivity products to identifiy the hook echo or bow echo patterns, and the velocity products for mesocyclone patterns as the characteristic of the Puting Beliung used radar product. The study required the Cengkareng C-Band raw data radar that was processed to produce CMAX, VCUT, and CAPPI (V) at 0.5 km, 1.0 km, and 1.5 km elevations overlay by HWIND. The CMAX and VCUT radar products are used to identify the cloud structure that caused Puting Beliung, by observed the highest reflectivity of the Puting Beliung-producing clouds. Then the CAPPI product overlay by HWIND is used to identify the movement of the wind which is suspected to be the beginning of the formation of a Puting Beliung at that location which is characterized by the presence of a mesocyclone pattern in the form of wind components and radial velocity. It was suspected that there was a wind rotating in the Central Jakarta area which indicated a Puting Beliung in the area. The analysis of this radar interpretation was then validated using satellite imagery to detect the cumulonimbus clouds forming the Puting Beliung. From this research, it is known that the Puting Beliung occurred around 08.12 UTC. The growth of cyclone-producing clouds occurred rapidly with a reflectivity value between 35 - 45 dBZ and wind speed up to 35 knots. Analysis of satellite imagery showed a significant decrease in cloud peak temperature so that the formation of convective clouds in the form of Cumulonimbus clouds indicates the phenomenon of the Puting Beliung. However, in this case study the Puting Beliung phenomenon is indicated as seen from the mesocyclone pattern of the rotating radial velocity component, and not from the hook echo or bow echo pattern.
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