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Davos, nestled high in the Swiss Alps within the canton of Graubünden, presents a unique geographic profile profoundly influencing its air quality. Situated at an elevation of 1,564 meters (5,131 feet), the town occupies a valley floor carved by the Landwasser River, surrounded by towering peaks exceeding 3,000 meters. This location within the Albula Alps creates a natural basin, which, while offering stunning views, can also trap pollutants under certain meteorological conditions. The surrounding landscape is dominated by coniferous forests and alpine meadows, contributing to a generally clean background air quality, but also susceptible to wildfire smoke during drier periods. Davos’s regional position is significant; it lies within a relatively sparsely populated area, far removed from major industrial belts. The closest significant urban centres are Chur and St. Gallen, both located down valley, minimizing direct industrial pollution transport. The urban–rural gradient is sharp, transitioning rapidly from the town’s built environment to extensive alpine pastures and wilderness. Agricultural activity in the lower valleys contributes some localized emissions, primarily related to livestock and fertilizer use, but these are generally minor compared to potential atmospheric conditions. The Landwasser River, while providing a visual amenity, doesn't significantly impact air quality, though its presence can influence local humidity and fog formation. The steep valley walls restrict airflow, a key factor in understanding Davos’s air quality dynamics.

Davos’s air quality exhibits a distinct seasonal pattern dictated by its alpine climate. Winter months (December-February) are often characterized by temperature inversions, where cold air becomes trapped in the valley floor beneath a layer of warmer air aloft. This inversion prevents vertical mixing, leading to a build-up of pollutants, particularly particulate matter from wood-burning stoves used for heating. Fog, common during winter, further exacerbates this issue by reducing dispersion. Spring (March-May) sees a gradual improvement as temperature inversions weaken and sunlight increases, promoting atmospheric mixing. However, snowmelt can temporarily increase humidity and contribute to localized haze. Summer (June-August) generally offers the best air quality, with strong solar heating driving vigorous vertical mixing and frequent precipitation cleansing the atmosphere. However, the risk of wildfire smoke drifting in from surrounding regions, particularly during drier years, remains a concern. Autumn (September-November) presents a transitional period; cooler temperatures can trigger weak inversions, and the onset of autumn rains can initially improve air quality before a return to more stable conditions. Sensitive groups, such as individuals with respiratory conditions and young children, should exercise caution during winter months, limiting outdoor activity on days with persistent fog or noticeable haze. During wildfire season, monitoring local air quality reports and avoiding strenuous outdoor exercise is advisable. The town’s reliance on wood for heating necessitates responsible burning practices to minimize particulate emissions throughout the colder months.