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Douar Ain Maatouf, nestled within the Fès-Meknès region of Morocco, occupies a geographically significant position at approximately 34.4352° latitude and -4.5566° longitude. The settlement’s location, with an elevation of around 700 meters above sea level, places it within a gently sloping terrain characteristic of the Middle Atlas mountains' foothills. This elevation, while offering some degree of natural ventilation, can also contribute to temperature inversions, a key factor influencing air quality. The surrounding landscape is a mosaic of agricultural land – primarily olive groves and cereal fields – interspersed with pockets of cedar and cork oak forests. This agricultural activity, while vital to the regional economy, introduces potential sources of particulate matter, particularly during harvesting and tilling seasons. Douar Ain Maatouf exhibits a clear urban–rural gradient; it’s a relatively small village, distinct from the sprawling urban agglomeration of Fès, yet close enough to be influenced by its activities. The proximity to Fès, approximately 25 kilometers to the northeast, means that industrial emissions and vehicular traffic from the larger city can occasionally impact local air quality. The absence of major rivers or lakes in the immediate vicinity limits the natural cleansing effect of water bodies, further emphasizing the importance of understanding local meteorological patterns and emission sources. The prevailing winds, generally from the northwest, play a crucial role in dispersing pollutants, but can also carry them from Fès.

Air quality in Douar Ain Maatouf follows a distinct seasonal pattern dictated by Morocco’s Mediterranean climate. The dry season, spanning roughly from April to October, typically sees lower overall pollution levels due to increased wind speeds and solar radiation, which aids in pollutant dispersion and photochemical degradation. However, dust storms, common during the late spring and summer months (May-July), can dramatically degrade air quality, introducing high concentrations of particulate matter. These storms originate from the Sahara Desert and are exacerbated by dry, unstable atmospheric conditions. Conversely, the cooler, wetter months (November to March) are characterized by increased humidity and frequent fog, particularly during December and January. This stagnant air, coupled with reduced solar radiation, can lead to temperature inversions, trapping pollutants near the ground and resulting in periods of poorer air quality. Agricultural burning, a traditional practice for land clearing and crop residue disposal, is most prevalent in the late autumn and early spring (October-November and March-April), contributing significantly to localized smoke and particulate pollution. Sensitive groups, including children, the elderly, and individuals with respiratory conditions, should exercise caution during dust storm events and periods of fog. Outdoor activities are generally more favorable during the windier months of spring and autumn, avoiding the peak dust storm season and the stagnant conditions of winter. The transition months of March and October present a particular challenge, requiring careful monitoring of local conditions and adherence to public health advisories.