Weather Alert in New Mexico
Blowing Dust Advisory issued February 17 at 10:08AM MST until February 17 at 8:00PM MST by NWS Midland/Odessa TX
AREAS AFFECTED: Eddy County Plains; Eastern Culberson County
DESCRIPTION: * WHAT...For the High Wind Warning, west winds 35 to 45 mph with gusts up to 65 mph. For the Blowing Dust Advisory, visibility between one-quarter and one mile in blowing dust. For the High Wind Watch, southwest winds 30 to 40 mph with gusts up to 60 mph possible. * WHERE...In New Mexico, Eddy County Plains. In Texas, Eastern Culberson County. * WHEN...For the High Wind Warning and Blowing Dust Advisory, until 8 PM MST /9 PM CST/ this evening. For the High Wind Watch, from Wednesday morning through late Wednesday night. * 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 is Sleet?
Home - Education - Precipitation - Sleet
Next Topic: Snow
Sleet is a form of precipitation in which small ice pellets are the primary
components. These ice pellets are smaller and more translucent than hailstones,
and harder than graupel. Sleet is caused by specific atmospheric conditions and
therefore typically doesn't last for extended periods of time.
The condition which leads to sleet formation requires a warmer body of air to be
wedged in between two sub-freezing bodies of air. When snow falls through a warmer
layer of air it melts, and as it falls through the next sub-freezing body of air
it freezes again, forming ice pellets known as sleet. In some cases, water
droplets don't have time to freeze before reaching the surface and the result is
freezing rain.
Next Topic: Snow
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
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