Weather Alert in New Mexico
High Wind Warning issued February 17 at 4:55AM MST until February 17 at 8:00PM MST by NWS Midland/Odessa TX
AREAS AFFECTED: Eddy County Plains; Northern Lea County; Central Lea County; Eastern Culberson County
DESCRIPTION: * WHAT...For the High Wind Warning, west winds 35 to 45 mph with gusts up to 65 mph expected. For the Blowing Dust Advisory, visibility between one-quarter and one mile in blowing dust expected. * WHERE...In New Mexico, Central Lea and Northern Lea Counties, and Eddy County Plains. In Texas, Eastern Culberson County. * WHEN...From 10 AM MST /11 AM CST/ this morning to 8 PM MST /9 PM CST/ this evening. * IMPACTS...Hazardous driving conditions due to reduced visibility. A sudden gust of wind could drop visibility to near zero instantly. 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: Slow down, use low-beam headlights, and leave plenty of distance between you and other vehicles. Use caution if flying low near the mountains as severe turbulence is possible. Use caution when driving as blowing dust may reduce visibility.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
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