Weather Alert in New Mexico
Wind Advisory issued February 18 at 5:13AM MST until February 18 at 8:00PM MST by NWS Albuquerque NM
AREAS AFFECTED: Northwest Plateau; Far Northwest Highlands; Northwest Highlands; West Central Mountains; West Central Highlands; San Francisco River Valley; Jemez Mountains; Upper Rio Grande Valley; Espanola Valley; Santa Fe Metro Area; Middle Rio Grande Valley/Albuquerque Metro Area; Lower Rio Grande Valley; Sandia/Manzano Mountains Including Edgewood; Estancia Valley; South Central Highlands; Upper Tularosa Valley; San Agustin Plains and Adjacent Lowlands
DESCRIPTION: * WHAT...Southwest winds 25 to 35 mph with gusts up to 55 mph expected. * WHERE...Portions of western and central New Mexico, including the Albuquerque and Santa Fe metro areas. * WHEN...From 11 AM this morning to 8 PM MST this evening. * IMPACTS...Gusty winds will blow around unsecured objects. Tree limbs may be blown down. Expect strong crosswinds on area roadways. * ADDITIONAL DETAILS...This afternoon and early evening, there is a moderately high probability of snow squalls along and west of the Tusas and Jemez Mountains capable of producing brief periods of near zero visibility, a flash freeze, and a quick inch or two of snow that will make driving treacherous.
INSTRUCTION: Take action to secure trash cans, lawn furniture, and other loose or lightweight outdoor objects. Dangerous driving conditions can be expected, especially for motorists in high profile vehicles.
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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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