Enhanced radar detectability allows radar observations of clear air up to a height of 5 km. Layered atmospheric structures above the top of the convective boundary layer are shown and a few mechanisms of their origin are discussed. Initiation of convection is demonstrated, and the parameters of convective plumes in central Oklahoma are presented. A transition from convective plumes to cumulus clouds is shown by combining radar and satellite observations.
All six base radar variables are measurable from non-precipitating clouds and could be ingested into atmospheric models. Fine microphysical structures of clouds are demonstrated with a WSR-88D. The radar derived wind fields in clouds can be ingested into the models. A mission for cloud detection across the NEXRAD fleet is proposed, which can help with studies from various climatic regions.

