Using collocated measurements of aerosol radiative properties and radiative fluxes, aerosol radiative forcing is estimated at a tropical urban site in India, located between the sub-continent and the Indian Ocean Experiment sites. Observed sun/sky radiance data are used to derive aerosol spectral optical depth, single scattering albedo , asymmetry parameter, precipitable water and total column ozone. These serve as inputs to a radiative transfer model, to estimate aerosol forcing at the surface, the top-of-the atmosphere and the atmosphere. During the dry season of 2001 and 2002 , these were found to be -33, 0 and 33 Wm-2, respectively. Using measured radiative fluxes during different aerosol loading conditions yield a surface forcing of -31 Wm-2. The surface forcing efficiency as computed from the two independent methods is found to be -88 and -84 Wm-2, respectively, while mean SSA at 500 nm is found to be 0.81.