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Silivri occupies a strategic position as the westernmost gateway of Istanbul, serving as a critical transition zone between the dense urban sprawl of the metropolitan center and the expansive agricultural plains of East Thrace. Situated along the northern coast of the Sea of Marmara, the district is characterized by a predominantly flat topography, with low-lying coastal plains that gradually merge into fertile hinterlands. This geography creates a dynamic urban–rural gradient where residential clusters coexist with intensive greenhouse farming and burgeoning industrial estates. The proximity to the sea is the primary driver of local air quality, as the prevailing westerly winds often sweep pollutants away from the coast, providing a refreshing maritime influence. However, the district is bisected by the D-100 highway, a major arterial route that introduces significant vehicular emissions into the local atmosphere. The surrounding landscape, marked by vast open fields and scattered industrial belts, means that air quality is heavily influenced by both mobile sources and stationary industrial emissions. Because the terrain lacks significant mountainous barriers, there is generally good ventilation; yet, during periods of atmospheric stability, pollutants can linger near the surface. The interaction between the moist maritime air and the inland terrestrial heat creates localized microclimates that dictate the dispersion of particulate matter. Consequently, Silivri’s air quality reflects a complex struggle between its natural coastal advantages and the pressures of increasing industrialization and transit-heavy infrastructure that characterize Istanbul's westward expansion.

The air quality narrative in Silivri follows a distinct seasonal rhythm dictated by the Sea of Marmara and regional meteorological shifts. During winter, the district often experiences temperature inversions, where cold air becomes trapped near the ground, concentrating pollutants from residential heating and heavy vehicle exhaust. This is the period of highest risk for sensitive groups, particularly those with respiratory conditions, as stagnant air prevents the dispersal of particulate matter. As spring arrives, the atmosphere clears, but the rise in temperature brings a surge of biological aerosols and pollen, which can exacerbate asthma. Summer is characterized by intense solar radiation and high temperatures, which facilitate the photochemical reaction of nitrogen oxides and volatile organic compounds to form ground-level ozone. While the cooling sea breezes provide relief along the coastline, inland areas may see ozone peaks during the hottest afternoons of July and August. Autumn represents a transitional phase; however, this season often sees a temporary spike in particulate levels due to traditional agricultural burning in the surrounding Thrace plains. For those seeking the cleanest air, late spring and early autumn are generally the most favorable windows for outdoor activities. Vital health guidance suggests that vulnerable populations should limit exertion during winter mornings when inversions are strongest and avoid midday outdoor exposure during summer heatwaves. By monitoring these seasonal patterns, residents can better navigate the interplay between Silivri’s maritime climate and the anthropogenic emissions that define its air quality.