Taourirt occupies a strategic position in northeastern Morocco's Oriental region, situated approximately 100 kilometers southwest of Oujda and 300 kilometers east of Fez. The city lies at an elevation of around 400 meters above sea level in the Guercif Basin, a transitional zone between the Middle Atlas Mountains to the west and the arid plains extending toward Algeria to the east. This basin geography creates a semi-arid environment where Taourirt serves as a crucial transportation hub, with major road and rail connections linking Morocco's interior to eastern border regions. The urban character reflects this transit function, with linear development along transport corridors blending traditional Moroccan architecture with modern commercial zones. Surrounding landscapes feature rolling hills and dry river valleys (wadis) that seasonally carry water, with the Moulouya River flowing approximately 30 kilometers to the north—a vital water source for regional agriculture but too distant to significantly moderate Taourirt's local climate. The city's air quality is influenced by its position in this basin, which can trap pollutants under stable atmospheric conditions, particularly during temperature inversions. While not part of Morocco's major industrial belts, Taourirt experiences urban pollution from vehicle emissions along its busy transport routes, occasional dust from surrounding semi-arid terrain, and seasonal agricultural burning in nearby farming areas. The urban-rural gradient shows decreasing pollution levels moving away from the concentrated commercial corridors toward more scattered settlements in the surrounding countryside.

Taourirt's air quality follows distinct seasonal patterns shaped by its semi-arid climate and basin geography. During winter (December-February), cooler temperatures and frequent temperature inversions trap pollutants near the surface, particularly in morning hours when vehicle emissions combine with residential heating sources. This season often sees the year's poorest air quality, with sensitive groups advised to limit outdoor activity during morning inversion periods. Spring (March-May) brings gradual improvement as increasing temperatures break up inversion layers, though occasional dust storms from the surrounding semi-arid plains can temporarily degrade air quality, especially during windy periods in April. Summer (June-August) offers generally better dispersion conditions with warmer temperatures creating more vertical mixing, though intense heat can occasionally lead to ozone formation from vehicle emissions. The driest months see reduced particulate matter except during rare dust events. Autumn (September-November) begins with relatively good air quality that gradually declines as temperatures drop and inversion conditions return, compounded by agricultural burning in surrounding farmlands during harvest periods. Throughout the year, wind patterns play a crucial role—northeasterly winds typically bring cleaner air from less populated areas, while southerly winds can transport dust from drier regions. Sensitive individuals should monitor local conditions particularly during winter mornings and spring dust events, considering indoor activity during peak pollution hours.