Data from: Limitations of separate cloud and rain categories in parameterizing collision-coalescence for bulk microphysics schemes

Warm rain collision coalescence has been persistently difficult to
parameterize in the bulk microphysics schemes used by weather forecast
models, climate models, and higher resolution models of the atmosphere.
The Arbitrary Moment Predictor (AMP) has been run in a variety of
configurations for collision-coalescence to investigate reasons for the
difficulty. The simulations suggest that the primary reason traditional
bulk schemes struggle with warm rain formation is the use of separate
cloud and rain categories. When the drop size distribution is represented
a single bimodal distribution rather than two separate unimodal
distributions, the simulation of cloud-to-rain conversion is substantially
improved. This dataset contains all of the simulation output and scripts
required to reproduce the results in the manuscript that support these
conclusions.