Weather Alert in West Virginia
Winter Storm Warning issued February 22 at 3:52AM EST until February 24 at 1:00AM EST by NWS Pittsburgh PA
AREAS AFFECTED: Eastern Tucker
DESCRIPTION: * WHAT...Heavy snow. Total snow accumulations between 9 and 15 inches, with locally higher totals possible. A few wind gusts to 45 MPH are possible Sunday night into Monday. * WHERE...Eastern Tucker County. * WHEN...Until 1 AM EST Tuesday. * IMPACTS...Near blizzard conditions are possible Sunday night into Monday, as visibilities may drop below 1/4 mile at times due to falling and blowing snow. Travel could be very difficult to impossible. The hazardous conditions will impact the Monday morning and evening commutes. Gusty winds could bring down tree branches.
INSTRUCTION: Persons should delay all travel if possible. If travel is absolutely necessary, drive with extreme caution and be prepared for sudden changes in visibility. Leave plenty of room between you and the motorist ahead of you, and allow extra time to reach your destination. Avoid sudden braking or acceleration, and be especially cautious on hills or when making turns. Make sure your car is winterized and in good working order. Please report snow or ice accumulations by calling 412-262-1988, posting to the NWS Pittsburgh Facebook page, or using X @NWSPittsburgh.
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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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