Cumulus Clouds (Cu)
Cu humilis
Smog BL Top Clouds
BL Top Clouds - Dust
Cu congestus I
Cu congestus II
Cu con praecipitatio
Con congestus IV
Con congestus V
Windshear
Cu ´magritteus`
Cu mediocris
Cu pileus
Cu arcus
Penetration
Tropical Cu
Cloudstreets
Tradewinds
Marine BL
Overview

 

 


Cumulus mediocris/congestus pileus


Cu_before.jpg, CuPileus1+2.jpg: The image Cu_before.jpg was taken around 7 p.m. at Crete near Finokalia. A cloud which resembles a leewave cloud occurs above the Cumulus mediocris in a short vertical distance. This veil-like cloud indicates that the air above the Cumulus mediocris is humid, i.e. near saturation so that cloud formation can easily occur. Later the Cumulus mediocris formed a cap which is called pileus. The affected area is marked in CuPileus1.jpg. CuPileus2.jpg is the same picture without the marking. A pileus cap is formed when humid air is lifted about a short vertical distance in a stable layered environment and condensation occurs. This lifting can for example be caused by ascending Cumulus cloud parts, which push the humid, but clear air above them by convection upwards. If the buoyancy of the Cumulus clouds below is large enough, the pileus can be completely penetrated. Mostly the remaining pileus cover drops once again hence it was formed in a stable atmospheric layering or the pileus is sucked into the Cumulus cloud. In both cases the pileus becomes invisible again. Also in the case of this cloud above Crete the pileus could be only noticed for few minutes. This means that a pileus can typically be only seen when one observes a convective cloud for a while.

Cu_pileus3.jpg: On this day several thunderstorm cells were formed between Hunsrueck and Mainz. The Cumulus congestus cloud shown here grew between 4.30 p.m. and 6 p.m. to a Cumulonimbus with strong precipitation, but without generating a thunderstorm. An anvil of another Cb cloud above the Taunus which extended over the ascending Cu congestus inhibited this development.

Pileus0-61.jpg: Here many, partly very similar images are presented, showing that the pileus comes up within a few minutes and also disappears again very quickly. The individual groups of pictures are related to a single cloud or different parts of a larger Cu congestus cloud cluster. Although the thumbnails look very similar, the full images give many details.

In some of the other chapters of the Cloud Gallery images of the pileus can be found (for example in chapter Wind shearing).

Cu_before.jpg, CuPileus1+2.jpg: S. Borrmann; North-eastern Crete, MINOS Field Campaign, 3 August 2001

CuPileus3.jpg: S. Borrmann, Rhinehesse, 30 May 2003, 5:32:28 p.m.

Iridescence1-5.jpg: S. Borrmann, J. Baehr, Nourlangie Rock, Kakadu National Park, NorthernTerritory, Australia, 3 December 2005, 3:25 p.m. local time

Pileus0-38.jpg: S. Borrmann; Route from Fortaleza to Quichada in North-eastern Brazil, 15 April 2005, 1 to 1:15 p.m.

Pileus39-46.jpg: see above, 1:53 to 1:55 p.m.

Pileus47-49.jpg: see above, 1:39 to 14:41 p.m.

Pileus50-56.jpg: see above, 2:41:40 to 2:43 p.m.

Pileus57-59.jpg: see above, 2:56 p.m.

Pileus60+61.jpg: see above, 2:39 to 3:05 p.m.