Weather Alert in Colorado

Recent Locations: Denver, CO  

Special Weather Statement issued March 15 at 2:18AM MDT by NWS Denver CO

AREAS AFFECTED: Jefferson and West Douglas Counties Above 6000 Feet/Gilpin/Clear Creek/Northeast Park Counties Below 9000 Feet; Elbert/Central and East Douglas Counties Above 6000 Feet

DESCRIPTION: At 218 AM MDT, Doppler radar was tracking a snow squall along a line from 7 miles southeast of Kiowa to 6 miles south of Sedalia, or along a line from 36 miles west of Limon to 25 miles south of Denver, moving southeast at 30 mph. Locations impacted include... Castle Rock, Elbert, Elizabeth, Kiowa, Larkspur, Franktown, Greenland, Ponderosa Park, Perry Park, Castlewood Canyon, Fondis and Shamballa. Visibilities will drop quickly to less than a quarter of a mile in this snow squall. Interstate 25

INSTRUCTION: Monitor the weather situation closely and be alert for threatening weather conditions. Use extra caution if you must travel into or through this snow squall. Rapid changes in visibility and potentially slick roads are likely to lead to accidents. Consider delaying travel until the squall passes your location.

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Weather Topic: What are Stratus Clouds?

Home - Education - Cloud Types - Stratus Clouds

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

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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