Ōzu Weather
Loading current temperature, humidity, wind, and air quality context for Ōzu, Kumamoto, Japan.
Loading current temperature, humidity, wind, and air quality context for Ōzu, Kumamoto, Japan.
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Ōzu, nestled in the southern reaches of Kumamoto Prefecture, Japan, presents a unique geographic setting influencing its air quality. The city occupies a basin surrounded by the Shiroyama and Kuma mountain ranges, creating a natural bowl-like topography. This terrain, at an elevation of roughly 150-200 meters, significantly impacts air circulation, potentially trapping pollutants during periods of atmospheric stability. The Kuma River, a major waterway, flows through Ōzu, providing a vital freshwater resource but also contributing to humidity levels which can affect pollutant dispersion. While Ōzu isn’t a major industrial hub, the surrounding region features agricultural activity – particularly rice cultivation – and smaller-scale manufacturing. The urban-rural gradient is relatively sharp; the city centre gives way quickly to forested hillsides and agricultural lands. This proximity to natural areas generally benefits air quality, but seasonal agricultural practices, such as burning rice straw after harvest, can introduce localised particulate matter. The city’s location, shielded by mountains, also means it experiences less direct influence from long-range transport of pollutants from larger industrial areas along the coast. Understanding these geographical factors is crucial for interpreting Ōzu’s air quality patterns.
Ōzu’s air quality follows a distinct seasonal rhythm. Spring (March-May) often sees increased particulate matter from agricultural burning as farmers prepare fields for planting, coupled with pollen from local flora. Winds are typically moderate, aiding some dispersion, but temperature inversions can occur, trapping pollutants near the ground. Summer (June-August) brings the humid subtropical climate into full effect. The rainy season (Tsuyu) generally improves air quality through wet deposition, washing pollutants from the atmosphere. However, stagnant air masses can develop between rain events, leading to localised build-up of pollutants. Autumn (September-November) is often the clearest period, with cooler temperatures, lower humidity, and stronger winds. However, increased use of heating systems as temperatures drop can contribute to localised smoke. Winter (December-February) presents the most challenging conditions. Cold, dry air and frequent temperature inversions trap pollutants, particularly from residential heating sources. Fog is common, exacerbating particulate matter concentrations. Sensitive individuals – children, the elderly, and those with respiratory conditions – should limit strenuous outdoor activity during winter mornings and after agricultural burns. Monitoring wind direction is key; winds from agricultural areas can bring increased particulate matter.
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US EPA AQI
😊 Good
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