Friday the 13th Hailstorm in the Province of Bulacan, Philippines (13 August 2021): A Case Study

IF 2.2 4区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES
Generich H. Capuli
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Abstract

This case study presents a thorough investigation of the environmental setup that led to the hail-producing severe storm that impacted the municipality of Norzagaray and City of San Jose Del Monte, including other nearby areas, in the province of Bulacan on the afternoon of August 13, 2021. During this period, 2–5 cm and potentially as large as ~8 cm diameter hail was reported over these locations of Bulacan. For this purpose, the combination of HIMAWARI-8 AHI, PLDN and its flash counts, and meteorological indices; synoptic, thermodynamic, and kinematic indices, calculated from the ERA5 reanalysis are utilized to understand the nature of the hail event. In the morning, the pre-convective environment was comprised by a warm inversion layer that inhibited storm initiation, until the arrival of ample moisture and convective heating in the afternoon. By the afternoon, model sounding analysis revealed that the environment transitioned into uncapped profile with steep low-level lapse rate owing to warm, moist south-westerly wind flow from the Manila Bay in the lower troposphere and north-easterlies aloft crossing the SMMR induced by a weak low-pressure system located in the eastern Philippine Sea, with minimal turning on the wind profile. This promoted low-level convergence within the area of interest and build up of instability. The updraft associated with convectively unstable atmosphere, sufficient cloud-layer bulk shear, and storm nudging at its maturing phase countered entrainment-driven dilution and aided the growth of ice crystals by rapid collection of supercooled cloud liquid particles, which ultimately led to formation of hailstones.

菲律宾布拉干省13号星期五冰雹天气(2021年8月13日):个案研究
本案例研究对导致2021年8月13日下午影响布拉干省诺扎加雷市和圣何塞德尔蒙特市(包括其他附近地区)产生冰雹的强风暴的环境设置进行了彻底调查。在此期间,布拉干这些地区报告了直径2-5厘米和可能大至8厘米的冰雹。为此,将HIMAWARI-8 AHI、PLDN及其闪数与气象指数相结合;利用ERA5再分析计算的天气、热力学和运动学指数来了解冰雹事件的性质。在上午,对流前环境由一个温暖的逆温层组成,该逆温层抑制了风暴的形成,直到下午充足的水汽和对流加热到达。到下午,模式探测分析显示,由于来自对流层下部马尼拉湾的暖湿西南风流和位于菲律宾海东部的弱低压系统诱导的东北气流穿过SMMR,风廓线转向极小,环境转变为低空递降率陡的无顶廓线。这促进了有关领域内的低水平趋同,并造成了不稳定。上升气流与对流不稳定的大气、充足的云层体切变和成熟阶段的风暴推动有关,抵消了夹带驱动的稀释作用,并通过快速收集过冷云中液体颗粒来帮助冰晶的生长,最终导致冰雹的形成。
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来源期刊
Asia-Pacific Journal of Atmospheric Sciences
Asia-Pacific Journal of Atmospheric Sciences 地学-气象与大气科学
CiteScore
5.50
自引率
4.30%
发文量
34
审稿时长
>12 weeks
期刊介绍: The Asia-Pacific Journal of Atmospheric Sciences (APJAS) is an international journal of the Korean Meteorological Society (KMS), published fully in English. It has started from 2008 by succeeding the KMS'' former journal, the Journal of the Korean Meteorological Society (JKMS), which published a total of 47 volumes as of 2011, in its time-honored tradition since 1965. Since 2008, the APJAS is included in the journal list of Thomson Reuters’ SCIE (Science Citation Index Expanded) and also in SCOPUS, the Elsevier Bibliographic Database, indicating the increased awareness and quality of the journal.
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