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We had a huge storm last night. This was the beginning of it. It literally went from 0 to 60 in 5 minutes. The sky was clear just minutes before the beginning of the film and by the end of it the sky was about to burst open. Only a couple minutes of footage was missing from 'start' to 'finish' which I edited out because I had to wipe my camera lens and re-adjust.
Monsoon isn't like a normal storm, it's quite amazing and this area in Arizona is the only place in North America that has one. For more information on the monsoon see below or in the pin commented, as I don't think all the info will fit here.
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The Sonoran Desert Monsoon
The word monsoon refers to a system of winds that changes seasonally, bringing wet and dry periods to a region. In the Sonoran Desert, the summer monsoon consists of winds from the sea flowing inland to fill the partial vacuum created by rising continental air warmed by the summer sun.
These winds bring moisture. The belt of westerlies shifts north in the summertime so that the Pacific high sits around 40 latitude, allowing moist air from the Pacific off of Baja California to move into the region.
These westward-moving winds actually circle around into the area and often reach the Sonoran Desert as southeasterly winds. This is one reason people in the past assumed that monsoon moisture comes from the Gulf of Mexico.
Recent studies, however, lead many meteorologists to believe that most moisture from the southeast is drained by the 6500 foot (1980 m) Mexican Sierra Madre and so doesn't reach the Sonoran Desert. This issue is yet unresolved.
Once Pacific moisture reaches our area, usually in July, the increased humidity means we really begin to feel the heat. If June has proceeded as usual, the desert surface is very hot, causing the moist air moving in to expand and rise. The hot air rising off the desert floor moves upward in great columns called thermals, which can be three to five miles (5 to 8 km) in diameter. Broader areas of cooler air separate the thermal columns, which is why thunderheads can be so wildely scattered.
The creation of thermals can be a violent business, and local updrafts can move at over fifty feet (15 m) per second. The strong convection upwards is usually matched by strong downdrafts which kick up sand and dust as they hit the land.
Above, the air cools as it rises, until at about 17,000 feet (5200 m) the moisture freezes. A growing thunderhead can tower 40,000 feet (12,000 m) or more, with the whole top containing a raging snowstorm a strange concept to a person broiling at ground level.
(Information taken from the desertmuseum.com and cont. below in the pinned comment)