Ground-based remote sensing scheme for monitoring aerosol–cloud interactions

Although this study focused only on warm-phase clouds, our findings regarding different cloud responses to aerosol perturbations between GCMs and satellite observations will

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

The number of aerosols that eventually activate into cloud droplets depends on the aerosol concentration, size distribution and chemical properties and on the updraft ve- locity,

Since we used the aerosol and cloud layers detected with the highest confidence for analysis (and thus providing the lowermost estimates of overlap frequency), we further in-

Operating two laminar flow DEG CPCs with di ff erent cut-o ff sizes together with other aerosol instruments, we looked at the growth rates of aerosol population in the CLOUD chamber

The spatial distribution of aerosol chemical com- position and the evolution of the Organic Aerosol (OA) fraction is investigated based upon airborne measurements of aerosol

Measured DOLP in the three polarimetric AirMSPI bands (circles) as a function of view zenith angle compared to results for the monomodal model with 0.06 µm median particle radius

In simulation SCAV- w the scavenging processes within the orographic cloud im- pact the aerosol size distribution by reducing the number and mass of unactivated aerosol particles..