On July 25, after days of storms, more than 3 inches of rain fell in six hours near Picacho Peak. Luckily, the canal is below the rest of the terrain in this area. That and the quick thinking of remote operators helped limit the damage.

No canal water was lost, and though there were some temporary turbidity issues downstream, scheduled water deliveries never missed a beat. And, unfortunately, it may be a harbinger of things to come. CAP canal must be able to withstand more I know. It might seem weird talking about the danger of flooding in a place that is only expected to get hotter and drier. But climate change is also expected to turn what precipitation we do get into a case of feast or famine. In this stage, the primary activity within the cell is pronounced vertical uplift. Warm moist air is lifted adiabatically and condenses to form cumulus-type cloud formations. As the updraft stage continues, the formation of towering cumulus begins.

Little or no precipitation occurs during this stage.

The second stage of thunderstorm development is the mature stage that is continue reading by both updrafts and downdrafts. Downdrafts are associated with air that is pulled downward by precipitation. Normally downdrafts will be found near the leading edge of the thunderstorm cell. The air descending from the thunderstorm will often hit the ground and be forced out ahead of the cell creating a gust front. The common desert term for such a phenomenon is haboob. Haboob: A lens-shaped dust wall generated from surface outflow see downburst from a mature thunderstorm cell.

The name comes from the Arabic word habb, meaning "wind. Their average duration is less than three hours.

The average maximum wind velocity is over 30 mph and dust may raise to heights exceeding feet. Localized pockets of intense downdrafts can create severe weather conditions called "downbursts". A "downburst" is a strong downdraft that induces an outward burst of damaging winds on or near the surface. Downbursts can be large, called a "macroburst" 2. Therefore, "macrobursts" and "microbursts" are severe conditions of downdrafts.

Cross section of a conceptual vortex ring model of a microburst Caracena, ; Downdrafts can be dry or wet. Dry downbursts will not necessarily show a solid perturbation from the base of the cloud to the characteristic curl. Instead, a dry downburst is generally only visible when the vertically descending winds hit the ground and pick up substantial quantities of dust. These types of downbursts are common in Arizona and will be particularly evident during the early portion of the monsoon season when there is still little precipitation associated with thunderstorms. Wet downbursts, on the other hand, have the characteristic precipitation curl tracing out the vortex-ring circulation that surrounds the concentrated downdraft within the rain shaft.

Most wet downbursts will describe a "foot shape" as the strong vertical winds carrying precipitation hit the ground and curl upwards. Gustnadoes Gustnadoes are features that seem to combine some of the characteristics of dust devils and tornadoes. In essence, a gustnado is a tornado-like vortex that appears to develop on the ground and extend will it ever rain in arizona again hundred feet upward. These vortices generally develop along the leading edge of an outflow boundary from a thunderstorm cell. Although generally of limited duration, the winds of gustnadoes can be strong enough to cause damage. Gustnadoes are often mis-identified as fires. For example, associated with the photograph below, team members identified a gustnado occurring along an outflow boundary near the town of Guadalupe.

Upon arrival in the Guadalupe area, no evidence of the feature was seen but follow-up discussion with the Guadalupe Fire Department found that the Fire Department had been called out in response to a report of "a downed airplane that caused a huge fire just south of town". Cautious driving in the afternoon on on Aug.

High winds from a storm the night before caused the downed trees and power outages.

Hundreds of homes in the area are still without power after high winds from a storm the night before caused the downed trees and power outages. Hundreds of homes in the area are still without power after high winds from a storm Monday evening caused the downed trees and power outages. Due to heavy rain in the past week, wildflowers were blooming in the area. This year is also the second most on record for days of precipitation in the season, with 23 days of measurable rain, according to Marvin Percha, meteorologist for the weather service.

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