Phra Phutthabat Weather
Loading current temperature, humidity, wind, and air quality context for Phra Phutthabat, Saraburi, Thailand.
Loading current temperature, humidity, wind, and air quality context for Phra Phutthabat, Saraburi, Thailand.
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Phra Phutthabat, nestled in Saraburi Province, Thailand, occupies a unique geographic position within the central plains. The city’s name, meaning ‘Buddha’s Footprint’, hints at its historical and spiritual significance, drawing pilgrims and contributing to a localized economic activity. The terrain is characterized by gently rolling hills transitioning into the flatter Chao Phraya River basin, with an elevation around 78 meters. This location, while not directly on the river, places it within a region heavily influenced by the river’s hydrological cycle and agricultural productivity. Surrounding the urban core are extensive rice paddies and agricultural lands, typical of central Thailand. While not a major industrial hub itself, Phra Phutthabat is situated within reach of industrial zones in Saraburi and Ayutthaya provinces, potentially contributing to regional air pollution transport. The urban-rural gradient is relatively sharp; the city centre is compact, quickly giving way to agricultural landscapes. This proximity to agricultural practices introduces potential sources of particulate matter from burning activities and fertilizer use. The prevailing winds, influenced by the monsoon patterns, play a crucial role in dispersing or concentrating pollutants, impacting local air quality. The city’s relatively sheltered position within the landscape can sometimes exacerbate pollution episodes by limiting natural ventilation.
Phra Phutthabat experiences a distinct tropical monsoon climate, shaping its air quality patterns throughout the year. The cool, dry season (November to February) generally offers the best air quality, with lower temperatures and winds aiding dispersion. However, agricultural burning to prepare fields after the harvest can cause localized spikes in particulate matter. The hot season (March to May) sees rising temperatures and stagnant air, leading to increased ground-level ozone formation and a build-up of pollutants. This period is often associated with haze from regional biomass burning. The southwest monsoon arrives in June, bringing heavy rainfall and improved air quality through atmospheric cleansing. However, increased humidity can also promote secondary pollutant formation. September and October, during the transition period, can experience fluctuating conditions, with lingering moisture and potential for localized flooding impacting pollutant dispersion. Sensitive groups – children, the elderly, and those with respiratory conditions – should be particularly cautious during the hot season and periods of agricultural burning. Monitoring wind direction is crucial; winds from the west and northwest often carry pollutants from larger industrial areas. Avoiding strenuous outdoor activity during peak heat and periods of visible haze is advisable.
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