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Jabonga is situated in the northern reaches of the Agusan del Norte province on the island of Mindanao, serving as a vital agricultural hub within the Caraga region. The municipality is characterized by a diverse landscape where rolling hills transition into fertile alluvial plains, deeply influenced by its proximity to the expansive Agusan Marsh and various river tributaries. This undulating terrain creates a complex microclimate; the valley areas can occasionally trap surface-level pollutants during stagnant air events, while the higher elevations benefit from consistent breezes. The urban character of Jabonga is predominantly rural, with a low-density settlement pattern that prevents the formation of intense urban heat islands common in larger Philippine cities. However, the surrounding landscape is dominated by extensive coconut plantations and rice paddies, creating a distinct urban-rural gradient where air quality is primarily influenced by organic emissions rather than industrial smog. Because it lacks a dense industrial belt, the primary pollutants are particulate matter from agricultural activities and road dust. The proximity to dense tropical vegetation acts as a natural carbon sink, helping to mitigate overall greenhouse gas concentrations and filtering the air. However, the town's position within a basin-like structure means that during periods of low wind speed, smoke from residential cooking and small-scale farming can linger, slightly elevating the concentration of fine particulates across the central residential clusters and the municipal core, which occasionally affects the clarity of the local atmosphere.

In Jabonga, air quality is governed by the tropical cycle of the wet and dry seasons rather than four temperate quarters. During the dry season, typically spanning from December to May, the region experiences the Amihan or Northeast Monsoon. This period often sees a peak in particulate matter as the drier soil leads to increased road dust and the practice of burning agricultural residues becomes more common. Temperature inversions may occur during cool mornings, trapping smoke from biomass burning close to the ground, which can irritate the lungs of sensitive groups. Conversely, the wet season, from June to November, is dominated by the Habagat or Southwest Monsoon. This period is characterized by frequent, heavy precipitation that effectively scrubs the atmosphere, washing away suspended particulates and significantly lowering pollutants. Consequently, air quality is generally at its cleanest during these months. For residents and visitors, the peak of the dry season, particularly March and April, is the time to exercise caution. People with asthma or chronic obstructive pulmonary disease should limit prolonged outdoor exertion during these hazy mornings. The most favorable months for outdoor activities are the transition periods or the rainy season, provided the weather is clear. Health guidance emphasizes staying hydrated and wearing masks during peak burning months to avoid respiratory distress. By monitoring the wind patterns and seasonal shifts, the community can better manage exposure to the episodic spikes in smoke and dust that define the regional atmospheric narrative throughout the year.