Weather Alert in New Mexico
Blowing Dust Advisory issued February 16 at 11:52AM MST until February 17 at 10:00PM MST by NWS Midland/Odessa TX
AREAS AFFECTED: Eddy County Plains; Northern Lea County; Central Lea County; Eastern Culberson County
DESCRIPTION: * WHAT...For the Blowing Dust Advisory, visibility between one-quarter and one mile in blowing dust expected. For the High Wind Warning, southwest winds 30 to 40 mph with gusts up to 65 mph expected. * WHERE...In New Mexico, Central Lea and Northern Lea Counties, and Eddy County Plains. In Texas, Eastern Culberson County. * WHEN...From 5 AM MST /6 AM CST/ to 10 PM MST /11 PM CST/ Tuesday. * 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 Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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