“…The optical properties of the aerosol determine the particles' direct effects on the Earth's radiative balance and weather-climate change (Ramanathan et al, 2001;Eck et al, 2005;Myhre, 2009;Che et al, 2019a;Li et al, 2016). Aerosol optical depth (AOD) is one of the key measures of the total aerosol extinction effects on climate (Breon et al, 2002), and the extinction Ångström exponent (EAE), with spectral dependence, can be used to obtain the information about aerosol size distributions (Gobbi et al, 2007;Eck et al, 1999;Zheng et al, 2017). The aerosols' absorptivity depends on particle composition and is a key determinant to calculate the direct aerosol radiative effect (Haywood and Shine, 1995;Li et al, 2016), and the singlescattering albedo (SSA) is a parameter that has the spectral dependence to distinguish major aerosol particle types (Jacobson et al, 2000;Dubovik et al, 2002;Gelencser, 2004;Russell et al, 2010;Giles et al, 2012).…”