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Nowogard, nestled within the Zachodniopomorskie Voivodeship of Poland, occupies a geographically significant position within the Pomeranian Lake District. Located approximately 60 kilometers southeast of Szczecin, the region’s largest city, Nowogard’s urban character is distinctly that of a market town, retaining a strong connection to its agricultural roots while experiencing gradual suburban expansion. The city sits on a gently undulating terrain, characterized by low hills and fertile plains, a legacy of glacial activity during the Pleistocene epoch. Its coordinates (53.6667, 15.1167) place it within a landscape dominated by forests, lakes, and agricultural fields, creating a clear urban–rural gradient. The nearby Drawsko Lake District, a network of interconnected lakes and waterways, influences local microclimates and contributes to humidity levels. While not directly bordering a major river, the proximity to smaller streams and drainage channels affects local hydrology. The surrounding landscape is primarily agricultural, with extensive fields of grain and rapeseed, interspersed with patches of deciduous forest. This agricultural activity, combined with the presence of smaller industrial enterprises within the town and surrounding villages, contributes to localized pollution sources. Nowogard’s elevation, relatively low at around 60 meters above sea level, can exacerbate the trapping of pollutants during periods of temperature inversion, particularly in the autumn and winter months. The regional position, bridging agricultural zones and the larger urban center of Szczecin, means it experiences a blend of rural and urban influences on air quality.

Nowogard’s air quality experiences a distinct seasonal cycle heavily influenced by meteorological conditions. Spring (March-May) sees a gradual improvement as temperatures rise and wind speeds increase, dispersing accumulated pollutants. However, agricultural activities, such as fertilizer application and field burning (though increasingly regulated), can contribute to localized spikes in ammonia and particulate matter. Summer (June-August) generally offers the best air quality, with consistent winds and higher temperatures promoting dispersion. However, prolonged periods of hot, still weather can lead to ozone formation, particularly during heatwaves. Autumn (September-November) presents a more complex picture. As temperatures cool, the likelihood of temperature inversions increases, trapping pollutants near the ground. Agricultural activity ramps up again, contributing to emissions. Fog, common during this season, further exacerbates the problem by reducing visibility and hindering pollutant dispersal. Winter (December-February) typically sees the poorest air quality. Cold temperatures, frequent temperature inversions, and reduced wind speeds create stagnant atmospheric conditions. Residential heating, often reliant on solid fuels like coal and wood, significantly contributes to particulate matter pollution. Sensitive groups, including children, the elderly, and individuals with respiratory conditions, should limit outdoor activity during periods of low visibility and stagnant air, particularly in the mornings and evenings. During the colder months, ensuring proper ventilation while heating is crucial to minimize indoor air pollution from combustion byproducts. Spring and autumn require vigilance regarding agricultural emissions and potential inversions.