Weather Alert in Colorado

Recent Locations: Tipton, MI   Holstein, NE   Elbert, CO  
Current Alerts for Elbert, CO: Red Flag Warning

Avalanche Watch issued February 24 at 10:51AM MST by NWS Denver CO

AREAS AFFECTED: Flat Tops; South and East Jackson/Larimer/North and Northeast Grand/Northwest Boulder Counties Above 9000 Feet

DESCRIPTION: AVABOU THE FOLLOWING MESSAGE IS TRANSMITTED AT THE REQUEST OF THE COLORADO AVALANCHE INFORMATION CENTER. ...AVALANCHE WATCH IN EFFECT FOR 5 AM WEDNESDAY TO 11 PM WEDNESDAY... * WHAT...Heavy snow and strong winds will result in HIGH (4 of 5) avalanche danger. * WHERE...Portions of the Front Range (Cameron Pass south to Berthoud Pass including Rocky Mountain National Park), the Elkhead Mountains, and the Flat Tops. * WHEN...Expect very dangerous avalanche conditions on Wednesday. * IMPACTS...Large and dangerous avalanches will be easy to trigger. Large avalanches will run naturally. PRECAUTION/PREPAREDNESS ACTIONS... Travel in backcountry avalanche terrain is not recommended on Wednesday. Avoid travel on and under slopes with a slope angle steeper than about 30 degrees. You can find more detailed information at colorado.gov/avalanche.

INSTRUCTION: N/A

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Weather Topic: What are Wall Clouds?

Home - Education - Cloud Types - Wall Clouds

Wall Clouds Next Topic: Altocumulus Clouds

A wall cloud forms underneath the base of a cumulonimbus cloud, and can be a hotbed for deadly tornadoes.

Wall clouds are formed by air flowing into the cumulonimbus clouds, which can result in the wall cloud descending from the base of the cumulonimbus cloud, or rising fractus clouds which join to the base of the storm cloud as the wall cloud takes shape.

Wall clouds can be very large, and in the Northern Hemisphere they generally form at the southern edge of cumulonimbus clouds.

Next Topic: Altocumulus Clouds

Weather Topic: What are Altostratus Clouds?

Home - Education - Cloud Types - Altostratus Clouds

Altostratus Clouds Next Topic: Cirrocumulus Clouds

Altostratus clouds form at mid to high-level altitudes (between 2 and 7 km) and are created by a warm, stable air mass which causes water vapor to condense as it rise through the atmosphere. Usually altostratus clouds are featureless sheets characterized by a uniform color.

In some cases, wind punching through the cloud formation may give it a waved appearance, called altostratus undulatus. Altostratus clouds are commonly seen with other cloud formations accompanying them.

Next Topic: Cirrocumulus Clouds

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