Regional and monthly and clear-sky aerosol direct radiative effect (and forcing) derived from the GlobAEROSOL-AATSR satellite aerosol product

C.: Improvement of aerosol optical depth retrieval from MODIS spectral reflectance over the global ocean using new aerosol models archived from 30. AERONET inversion data and

C.: Improvement of aerosol optical depth retrieval from MODIS spectral reflectance over the global ocean using new aerosol models archived from AERONET inversion data and

The well- predicted aerosol quantities, such as aerosol number, mass composition and optical properties, and the inclusion of full aerosol-cloud couplings lead to

using the Extended Aerosol Inorganic Model (E-AIM) (Clegg et al., 1998; Wexler and Clegg, 2002), by summing the total amount of sulphate and ammonium present in the aerosol

fire aerosol radiative effect (RE) at TOA, radiative effects due to aerosol–radiation interactions (REari), due to aerosol–cloud interactions (REaci), surface-albedo changes (REsac)

aerosol optical depth (AOD) of the atmosphere, acoustic sounding of the boundary layer, laser sensing of the aerosol content in the troposphere and stratosphere, mea- surement of

In this paper, numerous key uncertain factors in the retrieval of aerosol optical depth (AOD) are articulated for some widely used and relatively long satellite aerosol

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