The southwest monsoon rainfall not only provides water and food security over the Indo-Gangetic Basin, it also plays an important role in reducing atmospheric pollution by removing ambient particles via wet deposition processes. In addition to rainfall, aerosol loading and its removal from ambient air are also governed by other meteorological parameters, such as the temperature, humidity, wind speed, and wind direction. To understand the effect of southwest monsoon withdrawal on aerosol loading over the Indo-Gangetic Basin, airborne particles (PM 10 size fraction) and meteorological parameters, including the temperature, humidity, rainfall, wind speed, and wind direction data were collected between July and October 2015 at Kanpur, India, which is a large industrial city in the central part of the Indo-Gangetic Basin. The study shows that withdrawal of the southwest monsoon since July 2015 increased the aerosol loading in the ambient air by up to 28, 43 and 152% during August, September, and October, respectively. The aerosol loading exceeded the ambient Indian National Air Quality Standard limit of 100 μg/m −3 just within 3 months. In addition to increased aerosol mass loading, the concentration of heavy metals (Cr, Ni, Cu, and Cd) in the aerosols also increased with monsoon withdrawal. The only heavy metal that did not show an increasing trend was Pb, which indicates that Pb is either coming from local source(s) or that Pb was not efficiently scavenged by wet deposition processes. In general, Cd, Pb, and Cu concentrations were 10−1500 times higher when compared to the upper continental crust and were mostly derived from coal-burning products. The study shows that southwest monsoon strongly influence the physiochemical properties of aerosols over the Indo-Gangetic Basin.