Weather Alerts for Colorado
1. Fire Weather Watch for: Elbert/Central and East Douglas Counties Above 6000 Feet; 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
2. Fire Weather Watch for: Fremont County Including Canon City/Howard/Texas Creek; San Luis Valley Including Alamosa/Del Norte/Fort Garland/Saguache; Northern El Paso County Including Monument and Black Forest; Southern El Paso County Including Fort Carson and Colorado Springs; Pueblo County Including Pueblo; Crowley County Including Ordway; Otero County Including La Junta and Western Comanche Grasslands; Kiowa County Including Eads; Bent County Including Las Animas; Prowers County Including Lamar; Baca County Including Springfield and Eastern Comanche Grasslands
3. Fire Weather Watch for: Huerfano County Including Walsenburg; Western Las Animas County Including Trinidad and Thatcher; Eastern Las Animas County Including Pinon Canyon
4. Fire Weather Watch for: Kit Carson County; Cheyenne
5. Red Flag Warning for: Huerfano County Including Walsenburg; Western Las Animas County Including Trinidad and Thatcher; Eastern Las Animas County Including Pinon Canyon
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Current U.S. National Radar--Current
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North America Water Vapor (Moisture)
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - 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
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