The exceptions include altostratus that has varieties but no species, towering cumulus and cumulonimbus that have species but no varieties, and nimbostratus has no species or varieties.
12.
The World Meteorological Organization and the American Meteorological Society do not recognize cumulus castellanus as a distinct species, but instead classify all towering cumulus clouds as Cumulus congestus.
13.
Though fog eventually burned off, towering cumulus clouds developed before the next possible landing time at 11 a . m ., delaying the return of the shuttle until Saturday.
14.
Low and vertical heaps of " cumulus ", " towering cumulus ", and " cumulonimbus " are made of larger water droplets ranging in radius from 0.005 to about 0.015 mm.
15.
Later that afternoon, towering cumulus formed, darkened and then clashed, sending down deafening thunder rolls and microbursts of rain and hail, as if you were straddling the precipice between heaven and hell.
16.
:The cloud is either a Towering cumulus cloud or a Cumulonimbus cloud, likely a Cumulonimbus calvus as it has not yet formed its " anvil top " seen on fully mature cumulonimbus clouds.
17.
Unlike the related phenomenon associated with severe thunderstorms, cold-air funnels are generally associated with partly cloudy skies in the wake of cold fronts, where atmospheric instability and moisture is sufficient to support towering cumulus clouds but not precipitation.
18.
In hamlet after hamlet along the coast, the usual scenic glory-- towering cumulus clouds and spectacular views-- is clouded by a harsh reality : majestic palm trees uprooted, wires crossed, neighborhoods that appear as if they were bombed out.
19.
As the two aircraft approached the Grand Canyon, now at the same altitude and nearly the same speed, the pilots were likely maneuvering around towering cumulus clouds, though flying VFR required the TWA flight to stay in clear air.
20.
Towering altocumulus, known as altocumulus castellanus, frequently signals the development of thunderstorms later in the day, as it shows instability and convection in the middle levels of the troposphere, the area where towering cumulus clouds can turn into cumulonimbus.
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