Cloud formation Two processes, acting together or individually, can lead to air becoming saturated: cooling the air or adding water vapor to the air. But.
European Solar “Dimming” and “Brightening” as a Diagnostic for Aerosol Simulation in GCMs
Boundary Layer Clouds. Intertropiccal Convergence Zone (ITCZ) Trade cumulus Transition Stratus and stratocumulus subsidence Trade wind inversion St &
