A review of measurement-based assessments of the aerosol direct radiative effect and forcing

Finally, direct shortwave climate forcing by atmospheric aerosols occurs when so- lar radiation is abundant and springtime Arctic Haze or summertime fire plumes

The model has been used to study the impact of aerosol direct radiative e ff ect on East Asian climate (Zhang et al., 2012a), direct radiative forcing of anthropogenic aerosols (Bond

For anthropogenic aerosols, a good correlation has been confirmed through the comparison of fine aerosol fraction contribution as measured by radiometer, impactor and

The main aerosol components produced from road, shipping and aircraft transport are: black carbon (or soot) which we will refer as BC, organic carbon (OC) and sulphate.. A recent

A.: Validation of AERONET estimates of atmospheric solar surface fluxes and aerosol radiative forcing by ground- based broadband measurements, J. P., Re- dondas, A., and Sasaki,

The direct aerosol radiative forcing (DARF) has been estimated for the clear-sky conditions over Delhi from January 2006 to January 2007 using Santa Barbara DISORT Atmospheric

to solve underestimation of the simulated dust deposition over the Antarctic through, for example, detailed sensitivity experiments for analyzing what important factors are to

We analyze aerosol optical depth (sulfate, BC, and OC), aerosol climate forcing (direct and indirect), and climate response (temperature, precipitation rate, liq- uid water path, and