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Scarborough, the capital of Tobago, occupies a strategically important coastal position on the southwestern coast of the island, nestled within a dramatic landscape shaped by volcanic origins and relentless Caribbean trade winds. The town itself is relatively low-lying, situated at an elevation of approximately 30 meters above sea level, gently sloping upwards towards the verdant hills that dominate the island’s interior. This proximity to the Atlantic Ocean significantly influences local weather patterns and, consequently, air quality. Tobago’s surrounding landscape is a mosaic of lush rainforest, agricultural lands (primarily focused on citrus and cocoa cultivation), and pristine beaches. The urban–rural gradient is relatively sharp; Scarborough transitions quickly from a compact town centre to the surrounding agricultural and forested areas. While Tobago lacks large-scale industrial zones, the port of Scarborough handles shipping traffic, and occasional vessel emissions can impact localized air quality. The island’s location within the Lesser Antilles archipelago means it’s susceptible to airborne dust from the Sahara Desert, a phenomenon known as Saharan dust plumes, which can significantly degrade air quality. The prevailing northeast trade winds generally provide good ventilation, but topographic features can create localized areas of stagnant air, particularly during periods of reduced wind speed. The island’s volcanic soil contributes to a rich biodiversity, but also means potential for soil-borne particulate matter, especially during periods of heavy rainfall and erosion. The surrounding waters, including the Gulf of Paria, also influence humidity levels, which can affect the dispersion of pollutants.

Tobago’s tropical climate dictates a wet and dry season cycle, profoundly impacting air quality throughout the year. The dry season, typically running from February to May, often sees a reduction in rainfall and a corresponding increase in atmospheric stability. This can lead to temperature inversions, particularly in the evenings, where cooler, denser air becomes trapped beneath a layer of warmer air aloft. This inversion layer inhibits vertical mixing, trapping pollutants closer to the ground. Saharan dust plumes are also more frequent during this period, significantly reducing visibility and increasing particulate matter. The wet season, from June to November, brings frequent rainfall and higher humidity, generally leading to improved air quality as pollutants are washed from the atmosphere. However, heavy rainfall can also stir up soil particles, temporarily increasing dust levels. The transition months (May/June and November/December) are often characterized by variable conditions, with periods of both high dust and heavy rainfall. During the peak of the wet season (August-October), the increased cloud cover and rainfall provide a natural cleansing effect. Outdoor activities are generally most favourable during the wet season, particularly during the midday hours when rainfall is less likely. Sensitive groups, such as individuals with respiratory conditions and young children, should exercise caution during the dry season and when Saharan dust events are occurring, limiting prolonged outdoor exposure and taking necessary precautions like wearing masks. The interplay of trade winds, rainfall patterns, and Saharan dust events creates a dynamic air quality profile throughout the year.