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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.

Cloud bands of Cold Fronts in Warm Advection are very similar to those of Cold Fronts, but because of their relation to temperature advection are often…

A preferred area for the initial development of deep convection is the boundary of Dark Stripes in the WV images.

A Split Front is very similar to a Cold Front cloud band but shows a distinct double structure with cold (high) tops at the leading and warm (low) tops to…

Cloud bands of Cold Fronts in Cold Advection are very similar to those of Cold Fronts, but because of their relationship with temperature advection, they…

Cold Fronts are accompanied by synoptic scale multilayered cloud bands.