Santa Catalina Mountain Cloud Project
Overview and Live Camera
Background and Goals of the Project
Cloud Animations
The North American Monsoon and Mountain Thunderstorms
Personnel
Cloud Animations
Time-Lapse
Cloud Formation (Aug. 16, 2002)
This is an animation
of the sequence described in the Background and
Goals section. There is a low transition from
shallow to deep convection starting at about 9am
local time, and ending with a thunderstorm over
the mountains at about noon.
(Click on images below to view animation.)
Time-Lapse
Cloud Formation Part 1 (July 18, 2004) (Click on image
below to view animation.) Time-Lapse Rain Shaft Part 2 (July 18,
2004) (Click on image
below to view animation.) Time-lapse
Updraft (July 17, 2004) (Click on image
below to view animation.)
This is another example
of a slow transition from shallow to deep convection.
We're using wider angle lenses this year, and
the cameras also have a higher resolution. More
of the mountain is visible for reference. The
winds aloft are from the south on this day the
tops of the clouds are sheared off and drift over
the camera.
This sequence begins about
1/2 hour after the previous one ends. The large
cell on the left moves out of the frame, and the
clouds build again over the mountains. At this
time of day, there is generally widespread convection
and cells move into the frame from the west and
south. Toward the end of the sequence, the turbulence
of the cloud base and a bit of rotation are visible
during the heaviest rainfall.

(47 MB)
During the early stages
of development, the bases of the clouds tend to
be flat and uniform. This is due to the rising
air originating from the same level and having
similar amounts of moisture. Once the convection
develops and becomes organized, there is forced
lifting and the cloud bases become more chaotic.
In this animation a large convection cell moves
into the frame from the right. At about 17:15
(5:15pm local time) there is air being drawn into
the cloud base, with "fingers" forming
as water drops condense in the rising air.




