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Comparison of a global-climate model simulation to a cloud-system resolving model simulation for long-term thin stratocumulus clouds

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Fig. 1. Vertical profiles of (a) initial potential temperature and water vapor mixing ratio and (b) initial horizontal wind (u, v) velocity for the CSRM run.
Fig. 3. Time series of surface sensible (SH) and latent (LH) heat fluxes (W m −2 ) (a) for the CSRM run and (b) time series of LH surface fluxes for the CSRM-LH run.
Fig. 4. Time series of background aerosol number concentration (cm − 3 ) averaged over the MBL in the CSRM run.
Table 1. Summary of simulations.
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