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 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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