Unstructured cloud fields developing in areas of pronounced convergence.
Small scale lines of convective cells as a result of confluence in a land/sea system.
Lines of convective cells in advance of a Cold Front cloud band developing according to a diurnal cycle.
Development of convective cells and Cbs over mountain chains through confluence within a diurnal cycle.
A Comma is an active, mesoscale cloud spiral in the cold air behind frontal cloud bands, often with significant weather.
Small cloud cells arranged in parallel lines often found in cold air cloudiness.
A typical location for the development of Cbs and Mesoscale Convective Systems is at the leading edge of frontal cloud bands.
