Fig. 4: Water vapor mixing ratio response to aerosol perturbation in realistic shallow-convective clouds simulations. | Communications Earth & Environment

Fig. 4: Water vapor mixing ratio response to aerosol perturbation in realistic shallow-convective clouds simulations.

From: Boundary conditions representation can determine simulated aerosol effects on convective cloud fields

Fig. 4: Water vapor mixing ratio response to aerosol perturbation in realistic shallow-convective clouds simulations.

Vertical profiles of the domain and time mean a change in water vapor mixing ratio—qv, and b relative change in qv due to an aerosol perturbation (normalized to an order-of-magnitude increase in aerosol concentration). Same as Fig. 3 but focused only on the realistic simulations.

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