Weather Alert in New Mexico
High Wind Watch issued February 15 at 11:03AM MST until February 17 at 10:00PM MST by NWS Midland/Odessa TX
AREAS AFFECTED: Guadalupe Mountains of Eddy County; Eddy County Plains; Guadalupe Mountains Above 7000 Feet; Guadalupe and Delaware Mountains; Eastern Culberson County
DESCRIPTION: * WHAT...Southwest winds 35 to 40 mph with gusts up to 60 mph possible in the plains. West winds 45 to 55 mph with gusts up to 75 mph possible in the mountains. * WHERE...Guadalupe Mountains of west Texas and Southeast New Mexico, Eddy County Plains, and Eastern Culberson. * WHEN...From Tuesday morning through Tuesday evening. * IMPACTS...Travel will be difficult, especially for high profile vehicles like campers, vans, and tractor trailers. Blowing dust can reduce visibility suddenly to zero, especially in areas where bare fields exist. Severe turbulence near the mountains will be hazardous for low flying light aircraft.
INSTRUCTION: Monitor the latest forecasts and warnings for updates.
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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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