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- An elongated cloud band, visually similar to a roll cloud, usually appearing in the morning hours, when the atmosphere is relatively stable. Morning glories result from perturbations related to gravitational waves in a stable boundary layer. They are similar to ripples on a water surface; several parallel morning glories often can be seen propagating in the same direction.
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- Beaver(\'s) Tail, Billow Cloud, Feeder Bands, Inflow Bands, Inflow Stinger, Stratocumulus, T Rolls, Tail Cloud, Transverse Bands, Transverse Rolls