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Bangkok underwater: Record flooding after 48 hours of heavy rain, affected areas and forecasts

After nearly two days of heavy rainfall, Bangkok's canals overflow, inundating roads and neighborhoods. Discover which parts of the capital are flooded, the mechanisms that triggered this event, and short-term forecasts for the population.

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Rédaction Weather IA

samedi 26 septembre 2026 à 09:387 min
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Bangkok underwater: Record flooding after 48 hours of heavy rain, affected areas and forecasts
Bangkok in state of hydrological catastrophe

After nearly 48 hours of heavy rainfall, Bangkok's canals overflow, transforming main arteries into makeshift rivers. Over a third of the capital is submerged, with avenues like Ratchadamri and Sukhumvit now traversed on foot, while tens of thousands of residents are stranded in their homes. Satellite images from the Copernicus program show water sheets extending well beyond the traditional drainage network, revealing the magnitude of a crisis that goes beyond mere infrastructure problems.

Massive flooding in Bangkok: Affected areas and flood extent

The Chao Phraya, Khlong Saen Saep, and Khlong Phadung Krung Kasem canals have reached their maximum levels, inundating central districts of Bang Rak, Pathum Wan, and Dusit. Major roads, including Sukhumvit Road and Rama I, are completely submerged, requiring the use of boats or wading. Emergency services report that underground metro stations are closed, and hospital access routes are partially blocked, complicating medical interventions.

According to satellite data from Copernicus and ECMWF predictive models, the water surface continues to expand by about 15% every six hours as long as precipitation persists. Predictive models, fed by neural networks that assimilate real-time rainfall measurements, forecast that the flood peak could persist until the end of the weekend, followed by a slight retreat expected from the following Monday, provided atmospheric pressure stabilizes.

Meteorological mechanisms behind extreme rains

The phenomenon is explained by the interaction of a tropical wave from the Gulf of Thailand and a monsoon front that reinforced moisture input. Atmospheric data shows exceptional convergence of humid air flows, with water vapor rates above 30 g kg⁻¹, far beyond seasonal averages. This situation was amplified by a low surface pressure gradient, creating air mass stagnation and favoring continuous rainfall.

Ensemble models from ECMWF, enriched with weather radar and satellite data, indicate that the combination of abnormally high oceanic heat (≈31°C) and quasi-stationary atmospheric circulation generated a "train-storm" phenomenon, where several convection cells chained without interruption. This mechanism, rare but well-documented in climate studies, explains the persistence of intense rains over the same geographical area for several days.

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