Weather Alert in Colorado
High Wind Warning issued February 17 at 8:51AM MST until February 17 at 5:00PM MST by NWS Denver CO
AREAS AFFECTED: Larimer County Below 6000 Feet/Northwest Weld County; Northeast Weld County; Central and South Weld County; Morgan County; Central and East Adams and Arapahoe Counties; North and Northeast Elbert County Below 6000 Feet/North Lincoln County; Southeast Elbert County Below 6000 Feet/South Lincoln County; Logan County; Washington County; Sedgwick County; Phillips County
DESCRIPTION: * WHAT...West winds 30 to 40 mph with gusts up to 65 mph possible. * WHERE...Much of the eastern plains including, Briggsdale, Fort Morgan, Byers, Limon, Southern Lincoln County, Sterling, and Akron. * WHEN...Until 5 PM MST this afternoon. * IMPACTS...Damaging winds could blow down trees and power lines. Power outages are possible. Travel will be difficult, especially for high profile vehicles. Strong winds will likely lead to rapid fire growth of any new fire.
INSTRUCTION: People are urged to secure loose objects that could be blown around or damaged by the wind. Avoid outdoor burning or any activity that may cause sparks. The strong winds will likely fuel rapid fire growth.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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
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