Stupino Weather
Loading current temperature, humidity, wind, and air quality context for Stupino, Moskovskaya Oblast’, Russia.
Loading current temperature, humidity, wind, and air quality context for Stupino, Moskovskaya Oblast’, Russia.
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Stupino, situated in the Moskovskaya Oblast’ of Russia at coordinates 54.8833°N, 38.1000°E, occupies a geographically strategic, yet potentially air-quality-sensitive position. The city lies within the Oka-Don Plain, a gently undulating landscape characterized by morainic hills and river valleys. The elevation is relatively low, averaging around 160-180 meters above sea level, influencing local atmospheric circulation. The Stupino district is bisected by the Stupinushka River, a tributary of the Oka River, providing some natural ventilation but also potentially trapping pollutants during temperature inversions. Surrounding Stupino is a mix of agricultural land – primarily arable fields – and pockets of coniferous and mixed forests. Historically, the area was part of a significant industrial belt south of Moscow, and while some heavy industry has declined, remnants remain, contributing to localised emissions. The urban-rural gradient is fairly sharp; moving just a few kilometers outside the city limits brings a noticeable improvement in air quality. The proximity to Moscow, a major source of regional pollution, also impacts Stupino’s air quality, particularly through long-range transport of pollutants. The prevailing winds, generally from the west and southwest, can carry pollutants from the Moscow metropolitan area towards Stupino, exacerbating local conditions. This combination of terrain, land use, and regional influences creates a complex air quality profile.
Stupino experiences a continental climate, resulting in distinct seasonal air quality patterns. Winter (December-February) typically sees the poorest air quality, driven by increased heating demands from residential and industrial sources, coupled with stable atmospheric conditions and frequent temperature inversions that trap pollutants near the ground. Snow cover reflects sunlight, reducing dispersion. March and April bring a gradual improvement as temperatures rise and heating needs decrease, but dust from thawing roads can temporarily elevate particulate matter. Summer (June-August) generally offers the cleanest air, aided by higher temperatures, increased wind speeds, and rainfall which helps to wash pollutants from the atmosphere. However, periods of prolonged heat and stagnation can still lead to localised pollution build-up. Autumn (September-November) is a transitional period, with declining temperatures and increasing heating use leading to a gradual deterioration in air quality. Fog is common during autumn mornings, exacerbating particulate matter concentrations. Sensitive individuals – children, the elderly, and those with respiratory conditions – should limit strenuous outdoor activity during prolonged cold spells in winter and periods of fog in autumn. Monitoring local conditions and adjusting activity levels accordingly is crucial for protecting health. The spring thaw can also bring increased allergen levels, impacting respiratory health.
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