Weather Alert in New Mexico
Wind Advisory issued February 20 at 2:35AM MST until February 20 at 5:00PM MST by NWS Midland/Odessa TX
AREAS AFFECTED: Southern Lea County; Gaines; Van Horn and Highway 54 Corridor
DESCRIPTION: * WHAT...Southwest winds 25 to 35 mph with gusts up to 50 mph expected. * WHERE...In New Mexico, Southern Lea County. In Texas, Van Horn and Highway 54 Corridor, and Gaines County. * WHEN...From 11 AM MST /noon CST/ this morning to 5 PM MST /6 PM CST/ this afternoon. * IMPACTS...Strong winds will blow around unsecured objects and can cause reduced visibility in blowing dust.
INSTRUCTION: Winds this strong can make driving difficult, especially for high profile vehicles. Use extra caution and keep both hands on the steering wheel. Secure loose objects that could be damaged or blown away by strong winds. 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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