Surazh Weather
Loading current temperature, humidity, wind, and air quality context for Surazh, Bryanskaya Oblast’, Russia.
Loading current temperature, humidity, wind, and air quality context for Surazh, Bryanskaya Oblast’, Russia.
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Surazh, nestled within Bryanskaya Oblast’ in western Russia, occupies a relatively flat, low-lying position on the East European Plain. Its coordinates, 53.0167° N, 32.3833° E, place it within a temperate continental climate zone, characterized by significant seasonal temperature variations. The city is bisected by the Veselya River, a tributary of the Desna River, which influences local humidity and potentially traps pollutants during temperature inversions. Surazh is surrounded by a landscape dominated by mixed forests and agricultural land, primarily arable fields. The regional terrain is gently undulating, offering limited natural dispersion of airborne particles. While not a major industrial hub itself, Surazh’s proximity to larger industrial centres within Bryanskaya Oblast’ – particularly those related to machine building and chemical production – contributes to background pollution levels. The urban-rural gradient is relatively sharp; the city’s compact size is immediately bordered by agricultural fields and forested areas. This proximity means that prevailing winds can readily transport pollutants from surrounding agricultural activities, such as fertilizer application and crop burning, directly into the city. The soil composition, typical of the region, is predominantly chernozem, fertile black earth, which can become a source of dust during dry periods. This geographical setting fundamentally shapes Surazh’s air quality profile.
Surazh experiences a distinct seasonal air quality pattern. Spring (March-May) often sees a deterioration in air quality due to agricultural burning of crop residue and increased dust from thawing ground. Winds are variable, sometimes failing to adequately disperse pollutants. Summer (June-August) generally offers the cleanest air, with higher temperatures promoting atmospheric mixing and rainfall acting as a natural scrubber. However, prolonged heatwaves can lead to localized ozone formation. Autumn (September-November) brings a resurgence of pollution as heating systems are activated, burning coal and wood for warmth. This period is often marked by temperature inversions, trapping pollutants near the ground, particularly in the mornings and evenings. November is typically the most polluted month. Winter (December-February) is characterized by consistently low temperatures and stable atmospheric conditions, exacerbating the effects of heating emissions. Snow cover reflects sunlight, potentially increasing ozone concentrations. Fog is common, further reducing visibility and trapping pollutants. Sensitive groups – children, the elderly, and those with respiratory conditions – should limit outdoor activity during autumn and winter. Springtime agricultural practices also warrant caution. Monitoring wind direction and avoiding peak heating hours can help mitigate exposure.
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