Weather Alert in Nebraska
Winter Weather Advisory issued February 18 at 11:53AM CST until February 20 at 12:00AM CST by NWS Hastings NE
AREAS AFFECTED: Nance; Merrick; Polk
DESCRIPTION: ...WINTER RETURNS WITH ACCUMULATING SNOW AND GUSTY WINDS ON THURSDAY... * WHAT...Snow expected. Total snow accumulations between 2 and 4 inches. Northwest winds 20 to 25 mph, gusting 30 to 40 mph. * WHERE...Merrick, Nance, and Polk Counties. * WHEN...From 6 AM Thursday to midnight CST Thursday Night. * IMPACTS...Plan on slippery road conditions. The hazardous conditions could impact the Thursday morning and evening commutes. Gusty winds could lead to areas of blowing and drifting snow and reduced visibility. * ADDITIONAL DETAILS...A narrow band of moderate to heavy snow is forecast to develop Thursday morning and continue through the daytime hours, and perhaps into the evening. The area of heavy snow may be only 40 to 60 miles wide from north to south, so even slight shifts in storm track could lead to big changes in observed snowfall.
INSTRUCTION: Slow down and use caution while traveling. The latest road conditions for the state you are calling from can be obtained by calling 5 1 1.
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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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