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On Apr 28, 4:43*pm, Kemp wrote:
As always, comments are welcome. Kemp and Matt, Thanks to you both for this great video, though the reference to a pileus cloud forced me to do a Google search where I found (to save others the effort) the following: "A layer of cloud sometimes seen capping a cumulus cloud. The pileus layer forms when the cumulus cloud pushes a moist layer of air above it upwards, causing condensation in this layer. Eventually, the cumulus will grow into and penetrate the pileus cloud, after which the pileus may remain as a cloud skirt around the cumulus." An even better explanation, along with a nice still picture, was at http://www.stormeyes.org/tornado/SkyPix/pileus.htm "Pileus caps are made of ice crystals high in the troposphere. They form as a slab of air is shoved upward, in the shape of a dome or cap, just above a rapidly rising convective tower. Moisture in the dome condenses directly into an ice fog as the air rises and cools, forming the pileus. Next, the convection shoots right through the pileus layer. The lifted layer above the convective tower can't be too dry (must have high humidity), or the pileus cap won't develop." Thanks again. Marty WT |
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