Weather Alert in Ohio
Special Weather Statement issued February 6 at 7:20PM EST by NWS Pittsburgh PA
AREAS AFFECTED: Tuscarawas; Carroll; Columbiana; Coshocton; Harrison; Jefferson; Muskingum; Guernsey; Belmont; Noble; Monroe; Beaver; Allegheny; Washington; Greene; Hancock; Brooke; Ohio; Marshall; Wetzel; Marion; Monongalia
DESCRIPTION: Some areas of freezing drizzle are possible this evening, mixed at times with snow. The freezing drizzle may create a thin layer of icing on exposed surfaces and untreated roads. The risk of freezing drizzle is expected to end later this evening with the arrival of an arctic cold front. This front is forecast to bring bands of moderate to heavy snow showers, along with northwest wind gusts of 25 to 35 MPH. The snow showers may reduce visibility to a half-mile or less for brief periods and cause quick accumulation on untreated roads. Motorists are urged to use caution while driving this evening. Reduce speed and increase the distance between your vehicle and those that surround you.
INSTRUCTION: N/A
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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
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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