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Teresa, situated within the province of Rizal, serves as a critical transitional gateway between the hyper-urbanized expanse of Metro Manila and the rugged, verdant foothills of the Sierra Madre mountain range. Characterized by a rolling, undulating terrain, the municipality occupies a strategic position that bridges the gap between industrial corridors and rural landscapes. This geographic positioning is fundamental to its atmospheric profile. As the eastern periphery of the National Capital Region, Teresa often finds itself on the receiving end of urban-generated pollutants transported by prevailing winds. The town's elevation, rising gradually from the lowlands toward the mountain slopes, creates a complex topographical interface. Unlike the flat, stagnant basins of the central metro, Teresa's hilly landscape allows for better air dispersion in some areas, yet the valleys can experience localized trapping of particulates. The proximity to the massive industrial belts of neighboring towns in Rizal, combined with the heavy vehicular traffic traversing the arteries connecting the mountains to the city, creates a unique urban-rural gradient. While the presence of the Sierra Madre provides a natural buffer and a source of cleaner, oxygenated air, the municipality remains susceptible to the regional haze that drifts from the congested metropolitan center. Consequently, the air quality in Teresa is a delicate negotiation between the pristine influences of the highland forests and the anthropogenic emissions of the lowland urban sprawl, making its environmental health highly dependent on regional meteorological shifts and the intricate interplay of seasonal wind patterns within the Rizal province landscape and its topography.

In the tropical climate of Teresa, air quality patterns are primarily dictated by the alternation between the wet and dry seasons. During the dry season, typically spanning from November to May, air quality often undergoes noticeable degradation. As temperatures rise and the prevailing Amihan or northeast monsoon winds shift, the atmosphere can become more stable. This stability often leads to temperature inversions, particularly during the early morning hours, where a layer of warm air traps cooler, pollutant-laden air near the ground. This effect is most pronounced during the hotter months of March and April, when reduced rainfall means fewer natural scrubbing processes to wash particulates from the sky. Consequently, these months are often less favorable for strenuous outdoor activities. Conversely, the wet season, characterized by the Habagat or southwest monsoon from June to October, brings frequent rainfall that significantly improves air quality. The heavy downpours effectively cleanse the atmosphere of suspended particulates and aerosols, leading to much fresher air. However, during the transition periods, localized fog from the Sierra Madre foothills can occasionally mix with urban haze, creating periods of reduced visibility. For sensitive groups, such as children, the elderly, or those with respiratory conditions, it is advisable to monitor local environmental conditions closely during the dry season. Limiting prolonged outdoor exertion during peak heat and early morning hours in the dry months can mitigate exposure to concentrated pollutants that tend to settle in the lower valleys, especially during the early dawn hours when winds are lightest and air stagnates.