The Friday the 13th Hailstorm: A Rare Event
A severe hailstorm hits Bulacan, Philippines, on an unusual day.
― 4 min read
Table of Contents
On August 13, 2021, the province of Bulacan in the Philippines experienced a severe hailstorm that caught the attention of many. This storm was notable for its unusual occurrence on a day often associated with bad luck, leading some to humorously call it the "Friday the 13th Hailstorm." Hailstones reached sizes of 2 to 5 centimeters in diameter, with some reports suggesting sizes as large as 8 centimeters. Such events are quite rare in tropical regions, where one would typically expect warm rain rather than icy hail.
What Happened?
The storm struck in the afternoon, particularly affecting the municipalities of Norzagaray and the City of San Jose Del Monte. The hailstorm brought heavy rain and a downpour of ice pellets, which led to both excitement and concern among local residents. As social media became a platform for sharing experiences, reports of the hail's impact spread quickly, helping to document the unusual weather phenomenon.
How Hail Forms
To understand why hail fell in Bulacan, it's essential to know how hailstones are made. Hail is formed within Thunderstorms, particularly in strong ones. As warm air rises in the storm, it cools down in higher altitudes where temperatures dip below freezing. Water droplets in the storm are lifted high into the sky, where they freeze into ice crystals. These ice pellets can then be carried around by powerful winds within the storm. They gather more Moisture, growing larger until they become too heavy to be held aloft and eventually fall to the ground.
The Environment Leading Up to the Storm
On the morning of the hailstorm, the atmosphere in Bulacan was characterized by a warm layer of air that prevented thunderstorms from forming initially. But as the day progressed, moisture from the warm south-westerly winds blowing from Manila Bay mixed with rising heat, creating conditions ripe for a storm. The presence of a weak low-pressure system nearby helped to stir the atmosphere further, allowing the storm to become strong enough to produce hail.
A Meteorological Investigation
Scientists and meteorologists took a closer look at the storm to understand what happened. They used various tools and data sources, including satellites and lightning detection networks, to analyze the conditions leading to the hailstorm. They found that the low-level convergence—when different winds meet and force air upward—combined with strong Updrafts helped to make the storm potent enough to produce hail.
The Storm's Life Cycle
As the storm developed, it went through several stages. It started with the initial formation of clouds, followed by the growth of strong updrafts. During its peak, the storm exhibited characteristics typical of severe weather, including significant lightning activity and heavy precipitation. The hail was generated during this strong phase of the storm, where the combination of high moisture content, strong winds, and cold temperatures coalesced to create hailstones.
The Aftermath
The hailstorm caused various reactions among the local population. Social media posts flooded in with images and videos of the icy pellets, some jokingly referring to it as "nature's ice cream." However, this event also raised alarms about the potential damage that such storms could inflict on crops, vehicles, and property. The contrasting nature of the storm—bringing both fascination and concern—captured everyone's attention.
Climatology of Hail in the Philippines
Hailstorms in the Philippines are not common, making events like the one on August 13 noteworthy. Historically, the country has experienced some hailstorms, particularly in the northern regions. Research suggests that severe weather events, including hail, tend to occur during specific seasons, often aligned with the country's warm and dry months.
Climate Change
The Influence ofInterest in the effects of climate change on weather patterns is increasing. Scientists believe that shifts in temperature and atmospheric conditions due to climate change could lead to changes in the frequency and intensity of hailstorms. Understanding this relationship could be vital for predicting and preparing for future severe weather events.
Community Response
In the wake of the hailstorm, the local community participated in sharing experiences and collecting data about the event. This grassroots information gathering demonstrated the power of community and social media in understanding and responding to natural phenomena.
Conclusion
The "Friday the 13th Hailstorm" serves as a reminder of the unpredictable nature of weather, especially in a tropical setting like the Philippines. With ongoing research and community involvement, there is hope for better forecasting and understanding of future weather events. Who knows? The next storm might just be another quirky chapter in the Philippines’ weather story—hopefully, with a little less hail and a lot more sunshine!
Original Source
Title: Friday the 13th Hailstorm in the province of Bulacan, Philippines (13 August 2021): A Case Study
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 $\sim$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.
Authors: Generich H. Capuli
Last Update: 2024-12-15 00:00:00
Language: English
Source URL: https://arxiv.org/abs/2412.09307
Source PDF: https://arxiv.org/pdf/2412.09307
Licence: https://creativecommons.org/licenses/by/4.0/
Changes: This summary was created with assistance from AI and may have inaccuracies. For accurate information, please refer to the original source documents linked here.
Thank you to arxiv for use of its open access interoperability.
Reference Links
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- https://cds.climate.copernicus.eu/#!/home
- https://thredds.nci.org.au/thredds/catalog/catalogs/ra22/satellite-products/arc/obs/himawari-ahi/himawari-ahi.html
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