Weather Alert in Colorado
High Wind Warning issued March 11 at 11:50PM MDT until March 13 at 12:00PM MDT by NWS Denver CO
AREAS AFFECTED: South and East Jackson/Larimer/North and Northeast Grand/Northwest Boulder Counties Above 9000 Feet; South and Southeast Grand/West Central and Southwest Boulder/Gilpin/Clear Creek/Summit/North and West Park Counties Above 9000 Feet; Larimer and Boulder Counties Between 6000 and 9000 Feet
DESCRIPTION: * WHAT...West winds 35 to 50 mph with gusts 80 to 100 mph expected. * WHERE...Rocky Mountain National Park and the Medicine Bow Range, The Mountains of Summit County, the Mosquito Range, the Indian Peaks, and The Northern Front Range Foothills. * WHEN...From 4 AM Thursday to noon MDT Friday. * IMPACTS...Damaging winds may blow down trees and power lines, and scattered power outages are possible. Travel will be difficult, especially for high profile vehicles. This includes U.S. 40 over Berthoud Pass, I-70 from Golden to the Eisenhower Tunnel, and the Peak to Peak Highway. Strong winds may lead to rapid growth of any new fires, particularly below 7,500 ft.
INSTRUCTION: Drivers of high profile vehicles should consider delaying travel until winds subside Friday afternoon. People are urged to secure loose objects that could be blown around or damaged by the wind.
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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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