Hole Punch Cloud
Water temps in Clouds below but the water is not frozen. Unstable
Strong updraft a ting upon moist air at low altitudes. Unstable
Polar Stratosphere Clouds
Clouds in the winter polar stratosphere, reflecting ice crystals in the polar caps. Unstable. 15000-25000m above ground
Connected to the base Clouds, usually connected to strong thunder storms. Stable.
Collection of low marine Clouds. Stable
Mesoscale circulation with sea breezes to rol the cloud formations. Stable
A cellular pattern of pouches hanging underneath the base of a cloud. Unstable
Abused by a diffraction caused by small water droplets individuallly scattering light. Stable
Related to Undulavus Clouds by tending to dissipate with storm forming. Stable
Intense heat induces convection, which causes air mass to rise to a point of stability, usually with moisture. Stable
Morning Glory Clouds
Formed by wind squalls, with intense low-level wind shear, with a rapid increase in the vertical displacement of air parcels. Stable, located 100-200 meters above ground.
Formed by water ice crystals with a bright, pervasive polar cloud layer in the upper atmosphere. Unstable.
Created by atmospheric internal waves, created by a single air flow. Stable.
Formed at high altitudes, normally aligned perpendicular to the particular wind direction, stable.
Vertical displacement in the formation with sufficient moisture in the atmosphere. Stable.