Bualoi

Dissipated

Local time · Active from 24 Sep 2025 06:00 GMT+9 to 29 Sep 2025 19:00 GMT+7

Track map of Bualoi

Peak Category

Dissipated

Minimum Pressure

970 hPa

Maximum Wind Speed

126 km/h

Region

West Pacific

Key Events

Formation

24 Sep 2025 06:00 GMT+9

10.0°N, 133.2°E

Dissipation

29 Sep 2025 19:00 GMT+7

20.4°N, 101.6°E

Typhoon Bualoi: A Destructive Storm That Ravaged Southeast Asia in 2025

Introduction: The Moon-Sweeping Tempest

Typhoon Bualoi, named after a Thai dessert and known locally in the Philippines as Opong, emerged as one of the most destructive tropical systems of the 2025 Pacific typhoon season. This powerful storm carved a path of devastation through the Philippines and Vietnam before dissipating over Laos, leaving behind tragic loss of life and widespread destruction in its wake. The name "Bualoi" ironically means "moon" in Thai, contrasting sharply with the violent nature of this catastrophic weather event that would claim dozens of lives and destroy hundreds of thousands of homes across Southeast Asia.

Meteorological Evolution of Typhoon Bualoi

Genesis and Early Development

The origins of Typhoon Bualoi can be traced to a trough of low pressure that developed organized showers and thunderstorms north of Yap around September 22, 2025. By September 24, the system had organized sufficiently to be classified as a tropical storm, receiving the name Bualoi from the Japan Meteorological Agency while the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigned it the local name Opong. The system initially moved west-northwestward under the influence of a subtropical ridge, benefiting from warm sea surface temperatures and low vertical wind shear that promoted further organization.

Rapid Intensification and Peak Strength

Typhoon Bualoi underwent significant strengthening between September 26-27, transforming from a tropical storm into a powerful typhoon. By September 27, the Bualoi system had intensified to typhoon status with maximum sustained winds reaching 12th level (33 m/s). Meteorological analysis indicated that high sea surface temperatures in the central and northern South China Sea provided ample energy, while favorable upper-level outflow conditions and enhanced southwesterly monsoon flow contributed to the storm's organization and intensification.

The peak intensity of Typhoon Bualoi was reached on September 27-28, with the system achieving typhoon force winds of 35-40 m/s (12-13 level). Forecasters noted the possibility of the storm reaching strong typhoon level, with some models suggesting maximum intensities of 38-42 m/s (13-14 level) as it approached the southern sea areas of Hainan Island. The rapid strengthening of this Bualoi system was characteristic of 2025's active typhoon season, which saw multiple storms developing in quick succession.

Track and Movement Characteristics

The trajectory of Typhoon Bualoi displayed notably rapid movement, particularly as it entered the South China Sea. On September 27, the storm was moving westward at speeds of approximately 35 km/h, covering 240 kilometers in just six hours from 8:00 to 14:00. This accelerated motion continued as the system progressed toward Vietnam, with the storm maintaining a generally west-northwestward track throughout its lifecycle.

The Bualoi system followed a predictable path influenced by the positioning of the subtropical high-pressure system to its north. After forming east of the Philippines, the storm crossed through the central Philippine islands before emerging over the South China Sea. It then tracked toward the west-northwest, passing south of Hainan Island and ultimately making landfall in Vietnam.

Timeline of Critical Events

September 24: Formation and Initial Impact

The formative stage of Typhoon Bualoi began on September 24 when the Japan Meteorological Agency declared the system had developed into a tropical storm. Positioned approximately 1,420 kilometers east-southeast of Manila, Philippines, the initial system displayed maximum sustained winds of 18 m/s (65 km/h) with a central pressure of 1000 hPa. The newly formed storm was already moving westward at 10-15 km/h, setting it on a trajectory toward the Philippine archipelago.

September 26-27: Acceleration and Intensification

During this period, Typhoon Bualoi entered the South China Sea and began its rapid intensification phase. By September 26 at 17:00, the storm's center was located 950 kilometers east-southeast of Paracel Island, with sustained winds reaching 30 m/s. The Bualoi system dramatically accelerated to speeds of 35-40 km/h as it moved westward into the favorable environment of the South China Sea.

On September 27, the now powerful Typhoon Bualoi continued its rapid approach, positioned just 160 kilometers southeast of Paracel Island by 17:00. The storm had intensified further, with maximum winds reaching 33 m/s and central pressure dropping to 975 hPa. Forecast models consistently indicated the storm would continue toward Vietnam with possible slight strengthening before landfall.

September 28-29: Vietnamese Landfall and Dissipation

The culmination of Typhoon Bualoi's destructive path occurred in the early hours of September 29, when the storm made official landfall along the coast of Ha Tinh Province in central Vietnam. The Vietnam Meteorological Department reported that Bualoi came ashore with sustained winds of 30 m/s (11 level), making it a considerable typhoon at the time of landfall.

After moving inland, the Bualoi system rapidly weakened due to interaction with Vietnam's mountainous terrain. The storm degraded to a tropical depression within hours of landfall as it pushed westward toward Laos. By September 30, the remnants of Typhoon Bualoi had largely dissipated over eastern Laos, though its residual moisture continued to contribute to rainfall patterns across mainland Southeast Asia.

Impact Across Southeast Asia

Devastation in the Philippines

While tracking through the central Philippine islands, Typhoon Bualoi brought destructive winds and heavy rainfall to multiple regions. The storm's impact was particularly severe across Eastern Visayas and Bicol regions, where its passage caused widespread flooding and infrastructure damage. Although comprehensive casualty figures from the Philippines were not available in the search results, the storm's intensity suggests significant impacts on communities in its path.

Catastrophic Consequences in Vietnam

Vietnam bore the brunt of Typhoon Bualoi's destructive power, suffering tragic loss of life and widespread property damage. According to official statistics released by the Vietnamese government, the storm claimed 19 lives and left 21 others missing. The human toll was accompanied by devastating infrastructure damage, with reports indicating approximately 104,000 homes damaged or destroyed.

The agricultural sector suffered tremendously from the Bualoi onslaught, with over 9,400 hectares of rice and other crops flooded and more than 1,700 hectares of aquaculture operations destroyed. The storm's impact on infrastructure was equally severe, damaging transportation networks, irrigation systems, and flood control structures throughout Vietnam's central provinces.

Regional Effects and Peripheral Impacts

The influence of Typhoon Bualoi extended beyond its immediate track, with peripheral effects noted across Southeast Asia. Southern Chinese provinces, including Hainan, Guangdong, and Guangxi, experienced heavy rainfall and strong winds as the storm passed south of Hainan Island. The search results indicate that Bualoi's outer rainbands affected these regions, though the impacts were less severe than in Vietnam.

The remnants of Bualoi continued to generate precipitation across Laos and Thailand, with meteorological agencies warning of potential flooding and landslides in these countries following the storm's passage. The World Meteorological Center (Beijing) issued specialized forecasts highlighting the continued rainfall threat from the dissipating system across the Mekong River basin.

International Response and Cooperation

Multinational Forecasting and Warning Systems

The approach of Typhoon Bualoi triggered extensive international cooperation in meteorological forecasting and disaster preparedness. The World Meteorological Center (Beijing) played a particularly active role, issuing specialized forecasts on September 27 detailing the storm's anticipated impacts on the Indochina Peninsula. These products were shared with meteorological services throughout the region, including Vietnam's Meteorological and Hydrological Administration.

Regional collaboration was evident in the coordinated response to Bualoi. The Lao Meteorological and Hydrological Department utilized an early warning system developed in partnership with China to issue Bualoi alerts on September 24 and 26, disseminating critical information through their official "DMH LAO" mobile application. This international data sharing exemplified the growing cooperation in weather monitoring and disaster preparedness among Southeast Asian nations.

Chinese Meteorological Support

China's meteorological authorities provided significant support to regional efforts to monitor and prepare for Typhoon Bualoi. The World Meteorological Center (Beijing) supplied valuable forecast products, including 24-hour and 48-hour precipitation prediction maps for the Mekong River Basin, to the Lao meteorological department. These resources proved instrumental in helping vulnerable communities prepare for the storm's impacts.

The collaborative response to Bualoi continued a pattern established earlier in the 2025 typhoon season, during which Chinese meteorological agencies had partnered with counterparts in Vietnam, Laos, and Thailand to address multiple tropical systems including "Butterfly," "Wipha," "Jianyu," and "Hua Jiasha". This established network facilitated efficient information exchange as Bualoi approached the Southeast Asian mainland.

Meteorological Context and Climate Connections

2025 Typhoon Season Characteristics

Typhoon Bualoi developed during an exceptionally active period in the 2025 Pacific typhoon season. By September 24, the Northwest Pacific and South China Sea had already generated 20 named tropical systems, exceeding climatological averages for this point in the season. Meteorological analysts attributed this heightened activity to a combination of favorable environmental conditions, including stronger-than-normal subtropical highs positioned north and west of their typical locations, above-average sea surface temperatures, and favorable vertical wind shear patterns.

The development of Typhoon Bualoi represented the continuation of a pattern that had seen four tropical systems affect Guangdong Province within a 20-day period. This clustering of typhoon activity placed considerable strain on disaster response resources throughout Southeast Asia and highlighted the increasingly active nature of tropical cyclone formation in the region.

Notable Meteorological Characteristics

Several aspects of Typhoon Bualoi's behavior were particularly noteworthy from a meteorological perspective. The storm displayed unusually rapid translational speed, especially as it crossed the South China Sea, where it maintained forward motion of 35-40 km/h—significantly faster than average typhoon movement speeds. This accelerated progression limited the duration of impacts in any given location but also potentially enhanced asymmetric wind distribution.

The intensity evolution of Bualoi also demonstrated interesting characteristics, with the system maintaining strength despite its rapid movement—a challenge for many tropical cyclones. Forecast models successfully predicted the general intensification trend, though the storm's ultimate peak intensity slightly exceeded initial projections. The performance of these prediction systems for Bualoi represented continued improvement in tropical cyclone forecasting capabilities.

Aftermath and Recovery Efforts

Vietnamese Response to Disaster

Following the devastating passage of Typhoon Bualoi, Vietnamese authorities initiated comprehensive disaster response operations across affected provinces. The substantial casualty figures and widespread infrastructure damage necessitated large-scale relief efforts, particularly in hard-hit Ha Tinh Province where approximately 79,000 homes sustained damage. The Vietnamese government coordinated search and rescue operations while working to restore critical services in communities isolated by floodwaters and storm damage.

The agricultural devastation caused by Bualoi posed significant threats to food security and livelihoods in central Vietnam. With thousands of hectares of crops destroyed and aquaculture operations wiped out, recovery in the farming and fishing sectors was expected to require substantial time and resource investment. The Vietnamese government's response included immediate aid distribution while planning longer-term rehabilitation programs for affected agricultural producers.

Regional Recovery Challenges

The impacts of Typhoon Bualoi extended beyond immediate casualty and damage statistics, creating secondary challenges that complicated recovery efforts. Meteorological agencies warned that the storm's residual circulation could continue generating heavy rainfall for several days after the system's dissipation, maintaining elevated risks of flooding and landslides. These prolonged hydrological threats slowed the pace of recovery operations and increased the complexity of disaster response.

Infrastructure repair represented another significant dimension of the post-Bualoi recovery challenge. The storm's damage to transportation networks, including roads and bridges, impeded the delivery of assistance to isolated communities while complicating economic reactivation. The scale of housing damage also created urgent needs for temporary shelter solutions while permanent reconstruction was planned and implemented.

Conclusion: Lessons from a Destructive Storm

Typhoon Bualoi emerged as one of the most significant tropical systems of the 2025 Pacific typhoon season, leaving a tragic trail of destruction across Vietnam and the Philippines. The storm's rapid intensification, accelerated movement, and destructive landfall provided yet another example of the formidable challenges that tropical cyclones pose to Southeast Asian nations. The substantial casualties and widespread damage inflicted by Bualoi highlighted the continuing vulnerability of coastal communities to such events, despite improvements in forecasting and disaster preparedness.

The international response to Typhoon Bualoi demonstrated the value of regional cooperation in addressing transboundary natural hazards. The collaborative efforts between meteorological services across Southeast Asia facilitated more effective warnings and potentially saved lives despite the storm's ultimately destructive impacts. As climate patterns continue to evolve, the lessons learned from events like Bualoi will prove invaluable in building more resilient communities capable of withstanding future tropical cyclone threats.