Weather Alert in Colorado

Recent Locations: Denver, CO  

Severe Thunderstorm Warning issued June 5 at 1:52PM MDT until June 5 at 2:30PM MDT by NWS Pueblo CO

AREAS AFFECTED: Baca, CO; Prowers, CO

DESCRIPTION: SVRPUB The National Weather Service in Pueblo has issued a * Severe Thunderstorm Warning for... Northeastern Baca County in southeastern Colorado... Southeastern Prowers County in southeastern Colorado... * Until 230 PM MDT. * At 152 PM MDT, a severe thunderstorm was located 13 miles east of Two Buttes, or 28 miles northeast of Springfield, moving east at 25 mph. HAZARD...Tennis ball size hail and 60 mph wind gusts. SOURCE...Radar indicated. IMPACT...People and animals outdoors will be injured. Expect hail damage to roofs, siding, windows, and vehicles. Expect wind damage to roofs, siding, and trees. * Locations impacted include... Mainly rural areas of Northeastern Baca and Southeastern Prowers Counties.

INSTRUCTION: Anyone outdoors should move to shelter inside a well-built structure and stay away from windows. This storm is capable of producing dangerous hail and damaging winds. A Tornado Watch remains in effect until 800 PM MDT Thursday for a portion of southeast Colorado.

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Weather Topic: What are Altocumulus Clouds?

Home - Education - Cloud Types - Altocumulus Clouds

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

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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