Autumn 2017 | A SCM replaces advection from a dynamical core with forcing that approximates how the atmospheric column state changes due to large-scale horizontal winds. An atmospheric physics suite then calculates impacts to radiation, convection, microphysics, vertical diffusion and other physical processes as the forcing alters the column state. The SCM approach is conceptually simple, extremely quick to run (less than a minute on a laptop), and makes interpretation of results less ambiguous because it eliminates three-… Read More