Weather Alert in Colorado
Hydrologic Outlook issued May 8 at 1:24PM MDT by NWS Pueblo CO
AREAS AFFECTED: Alamosa, CO; Chaffee, CO; Conejos, CO; Costilla, CO; Custer, CO; Fremont, CO; Huerfano, CO; Lake, CO; Las Animas, CO; Mineral, CO; Rio Grande, CO; Saguache, CO
DESCRIPTION: ESFPUB Risk of enhanced runoff and elevated stream flows from rapid snowmelt ...EXISTING CONDITIONS... Recent storms have brought several inches of snow to mid to high elevations (8500'->10500') over the eastern San Juan and Sangre de Cristo Mountains of south-central Colorado, and along the Continental Divide of central Colorado. With upcoming precipitation, warming temperatures, and possible rain-on-snow for mid to high elevations, this region of Colorado is vulnerable to enhanced runoff and elevated stream flows from rapid snowmelt. ...PRECIPITATION... There is a roughly 35% chance of 0.1" or more of liquid precipitation over much of the area of concern later today (5/8) through Saturday afternoon. Precipitation in the form of rain could occur as high as 10,000 feet over the next two days. This elevated chance of rain-on-snow, along with warmer temperatures, could accelerate melting of new and existing snowpack. ...STREAMFLOW CONDITIONS AND RUNOFF FORECASTS... Streams and rivers in the area could see elevated flows of dangerously cold water over the next several days. Low lying areas and valley floors could see some minor inundation from snowmelt. Stay away from fast moving water, exercise caution near riverbanks and stay alert to watches and warnings from the National Weather Service. You can also find additional weather and water products and forecasts at the NWS Pueblo website at: Https://www.weather.gov/pub
INSTRUCTION: N/A
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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
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - 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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