Some are connected to a cumulus congestus
cloud, some to a cumuliform cloud and some to a cumulonimbus cloud.
Mechanisms to explain the shallow-to-deep transition include cold pool formation (Kuang and Bretherton 2006; Khairoutdinov and Randall 2006; Schlemmer and Hohenegger 2014), cumulus congestus moistening of the free troposphere (Waite and Khouider 2010), increasing cloud buoyancy (Wu et al.
By noon, cumulus congestus develops above the freezing level, begins to coalesce, and commences its propagation inland.
The Manaus network lends itself to the study of cumulus congestus cold pools and their role in the shallow-to-deep transition to deep precipitating cumulonimbus cells and their organization on the mesoscale.
(Cu) Cumulus--cumulos--: con una alta humedad y fuertes corrientes ascendentes, los cumulos adquieren gran tamano, se tornan grisaceos y originan tormentas y aguaceros; entonces se les denomina Cumulus congestus.
Esta medida, que se expresa en decibeles, se conoce como reflectividad y permite determinar la posicion exacta del tiempo perturbado, los cumulus congestus y los cumulonimbus.
A preliminary examination of infrared satellite images for the period showed a short east-to-west band of cumulus congestus
type clouds, with rain shower activity, near the area of the accident site.
When dry, heated ground air rises and meets moist tropical air, the moisture condenses into cloud droplets, which eventually form a cumulus congestus
cloud with billowy cauliflower shape.
In the initial stages of development the active plume first takes the form of a shallow dome-shaped cumulus congestus (Fig.
For [t.sub.4] < f < [t.sub.5], the heating profile is unchanged, the "mother" cloud slowly starts growing again into a cauliflower-shaped cumulus congestus (Fig.
4a) represents a cumulus congestus that shoots up as a tower and has a distinct plume head (simulated in the laboratory, see Fig.