Yonago Weather
Loading current temperature, humidity, wind, and air quality context for Yonago, Tottori, Japan.
Loading current temperature, humidity, wind, and air quality context for Yonago, Tottori, Japan.
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Yonago, nestled on the coast of the Sea of Japan in Tottori Prefecture, presents a unique geographic setting influencing its air quality. The city occupies a relatively flat coastal plain, bordered by the Daisen mountain range to the east. This terrain creates a funnel effect, potentially trapping pollutants during periods of stagnant air. Elevation rises quickly moving inland towards Daisen, creating a sharp urban-rural gradient. Yonago’s location directly on the Sea of Japan exposes it to maritime influences, including sea breezes and moisture-laden air. While not a major industrial hub, the surrounding Tottori Prefecture features agricultural zones – rice paddies and vegetable farms – which contribute to ammonia emissions, a precursor to particulate matter formation. Further east, limited industrial activity exists around Kurayoshi, but prevailing winds generally carry emissions away from Yonago. The city’s urban character is a blend of traditional Japanese architecture and modern development, with a relatively low population density compared to other Japanese cities. This lower density, however, doesn’t necessarily equate to cleaner air, as meteorological conditions often play a more dominant role. The coastal location also means susceptibility to salt spray, which can contribute to aerosol formation and affect air quality monitoring.
Yonago’s air quality follows a distinct seasonal pattern. Spring (March-May) often sees increased particulate matter from agricultural burning and dust storms originating from the Asian continent, carried by westerly winds. Pollen from cedar and cypress trees also contributes to discomfort for allergy sufferers, though this isn’t typically reflected in standard air quality indices. Summer (June-August) benefits from prevailing southwesterly sea breezes which help disperse pollutants, generally resulting in better air quality, though high humidity can exacerbate ozone formation on hot, sunny days. Autumn (September-November) is often the clearest period, with stable atmospheric conditions and reduced agricultural activity. However, temperature inversions can become more frequent, trapping pollutants near the ground. Winter (December-February) is typically the most challenging period. Siberian air masses bring cold, dry air and stagnant conditions, leading to a build-up of pollutants. Snowfall can temporarily cleanse the air, but also contributes to increased heating demands, and therefore emissions from residential sources. Sensitive groups – children, the elderly, and those with respiratory conditions – should limit strenuous outdoor activity during winter months and periods of stagnant air. Monitoring wind direction is crucial; onshore winds bring marine influences, while offshore winds can exacerbate pollution.
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