Weather Alert in Colorado
Flood Watch issued August 25 at 3:06AM MDT until August 26 at 12:00AM MDT by NWS Pueblo CO
AREAS AFFECTED: Northwestern Fremont County Above 8500Ft; Teller County/Rampart Range above 7500fT/Pike's Peak Between 7500 And 11000 Ft; Pikes Peak above 11000 Ft; Canon City Vicinity/Eastern Fremont County; Northern El Paso County/Monument Ridge/Rampart Range Below 7500 Ft; Colorado Springs Vicinity/Southern El Paso County/Rampart Range Below 7400 Ft; Pueblo Vicinity/Pueblo County Below 6300 Feet; Trinidad Vicinity/Western Las Animas County Below 7500 Ft
DESCRIPTION: * WHAT...Flash flooding caused by excessive rainfall continues to be possible. * WHERE...Portions of central, east central, and southeast Colorado, including the following areas, in central Colorado, Canon City Vicinity/Eastern Fremont County, Northwestern Fremont County Above 8500 Feet, Pikes Peak Above 11000 Feet and Teller County/Rampart Range Above 7500 Feet/Pikes Peak Between 7500 And 11000 Feet. In east central Colorado, Colorado Springs Vicinity/Southern El Paso County/Rampart Range Below 7400 Feet and Northern El Paso County/Monument Ridge/Rampart Range Below 7500 Feet. In southeast Colorado, Pueblo Vicinity/Pueblo County Below 6300 Feet and Trinidad Vicinity/Western Las Animas County Below 7500 Feet. * WHEN...From noon MDT today through this evening. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. * ADDITIONAL DETAILS... - http://www.weather.gov/safety/flood
INSTRUCTION: You should monitor later forecasts and be prepared to take action should Flash Flood Warnings be issued.
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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