Intercity Comparison of Aerosol Optical Depth and Modelled Surface Dust Concentrations across Seven West African Cities (2019–2025)

Aka Jacques Adon *

Equipe de la Physique pour l’Environnement, Laboratoire de Physique Fondamentale et Appliquée, Université Nangui Abrogoua, Abidjan 02 BP 801, Côte d’Ivoire.

Yao Tchetche

Equipe de la Physique pour l’Environnement, Laboratoire de Physique Fondamentale et Appliquée, Université Nangui Abrogoua, Abidjan 02 BP 801, Côte d’Ivoire.

Véronique Yoboué

Laboratoire des Sciences de la Matière de l’Environnement et de l’Energie Solaire (LASMES), UFR SSMT, Université Félix Houphouët-Boigny, 01 BPV 34 Abidjan, Côte d’Ivoire.

François-Xavier Djézia Bella Bouo

Equipe de la Physique pour l’Environnement, Laboratoire de Physique Fondamentale et Appliquée, Université Nangui Abrogoua, Abidjan 02 BP 801, Côte d’Ivoire.

*Author to whom correspondence should be addressed.


Abstract

Satellite aerosol optical depth (AOD) is widely used as a proxy for surface particulate pollution where ground monitoring is scarce, including in West Africa. This study tests whether this substitution holds for mineral dust by comparing MODIS MAIAC AOD (550 nm) with MERRA-2 modelled surface dust concentrations in seven cities (Dakar, Bamako, Niamey, Korhogo, Bouaké, Cotonou and Abidjan) over 2019–2025, on days matched by city and date, in November–March and April–October, using stationary-bootstrap 95 % confidence intervals. City rankings differ between the two quantities: Niamey has the highest surface dust in both windows, whereas the highest AOD occurs in Cotonou in November–March and in Dakar in April–October. Surface dust is higher in November–March in all seven cities, but AOD follows this seasonality only in Cotonou and Abidjan; it is opposite in Dakar and Bamako, and no clear contrast is detected elsewhere. The daily AOD–dust correlation is positive everywhere in November–March but becomes indistinguishable from zero in Abidjan in April–October. These dissociations persist even though MERRA-2 assimilates MODIS AOD. In April–October, AOD is less often available in the southern and central cities, where observed days are dustier than average. In practice, AOD captures part of the day-to-day dust variability within each city in November–March, but it should not be used to rank cities by surface dust concentration, to infer the seasonal cycle of surface dust, or as a proxy for surface dust on the Gulf of Guinea coast during the monsoon.

Keywords: Aerosol optical depth, MAIAC, MERRA-2 reanalysis, surface dust concentration, satellite sampling bias, air-quality proxy, intercity comparison, West Africa


How to Cite

Adon, Aka Jacques, Yao Tchetche, Véronique Yoboué, and François-Xavier Djézia Bella Bouo. 2026. “Intercity Comparison of Aerosol Optical Depth and Modelled Surface Dust Concentrations across Seven West African Cities (2019–2025)”. Physical Science International Journal 30 (6):82-96. https://doi.org/10.9734/psij/2026/v30i6997.

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