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Nabunturan, the capital of Davao de Oro province in the Philippines, occupies a strategically important location within the Mindanao region. Situated at approximately 7.6008° N, 125.9656° E, the city rests within a complex topography characterized by rolling hills and steep slopes, a consequence of its position within the Philippine Mountain Range. The elevation ranges from roughly 400 to 800 meters above sea level, influencing local climate and air circulation patterns. The surrounding landscape is predominantly rural, a mosaic of agricultural lands – primarily banana plantations and coconut farms – interspersed with dense secondary forests and pockets of primary rainforest. This agricultural intensity, while vital to the regional economy, contributes to potential sources of air pollutants, particularly from pesticide use and biomass burning during land clearing. Nabunturan’s proximity to the Pujada Bay, a significant body of water, offers some degree of coastal breeze influence, though the mountainous terrain often disrupts consistent airflow. The urban–rural gradient is relatively sharp; the city center exhibits a moderate concentration of commercial and residential buildings, while the periphery rapidly transitions to agricultural and forested areas. The city’s location, nestled within a valley, can exacerbate air pollution episodes, particularly during periods of stagnant air. The lack of expansive flatlands limits dispersion, and the surrounding mountains can trap pollutants, creating localized air quality challenges. The region's geology, with volcanic soils, also influences the potential for dust generation, especially during the dry season.

Nabunturan experiences a tropical climate with distinct wet and dry seasons, significantly impacting air quality dynamics. The wet season, typically spanning from June to November, brings frequent rainfall and high humidity, generally leading to improved air quality as precipitation washes away particulate matter and dilutes gaseous pollutants. However, intense storms can also stir up dust and debris, temporarily degrading air quality. The dry season, from December to May, presents a more complex scenario. Reduced rainfall and lower humidity contribute to a build-up of pollutants. Temperature inversions, common during the cooler months (January-February), trap cooler air near the ground, preventing the vertical dispersion of pollutants released from agricultural activities, residential wood burning, and limited industrial sources. The prevailing winds, often light and variable, further hinder pollutant dispersal. Fog, particularly in the mornings during the dry season, can also exacerbate air quality issues by trapping pollutants close to the ground. Agricultural burning, often practiced to clear land for planting, is a significant contributor to particulate matter pollution during the transition periods between seasons. Sensitive groups, including children, the elderly, and individuals with respiratory conditions, should exercise caution during the dry season, particularly during periods of fog or stagnant air. Limiting prolonged outdoor activity during these times and ensuring adequate ventilation indoors are recommended. The increased prevalence of dust during the dry season also necessitates the use of masks for those with allergies or asthma.