Weather Alert in Indiana
Winter Weather Advisory issued March 2 at 5:37AM EST until March 2 at 10:00AM EST by NWS Louisville KY
AREAS AFFECTED: Orange; Washington; Scott; Jefferson; Clark; Oldham; Trimble; Henry; Shelby; Franklin; Scott; Harrison; Bourbon; Nicholas
DESCRIPTION: * WHAT...Light snow, mixed with sleet and some freezing rain. Total snow accumulations of a coating to one inch possible. A light glaze on elevated surfaces is also possible. * WHERE...Portions of south central Indiana and east central and north central Kentucky. * WHEN...Until 10 AM EST this morning. * IMPACTS...Untreated roads, bridges, and overpasses may become slick. Plan on slippery road conditions. The Monday morning commute could be negatively impacted.
INSTRUCTION: Slow down and use caution while traveling. In Indiana, for Indiana Road Conditions please visit http://511in.org In Kentucky, for Kentucky Road Conditions please visit http://goky.ky.gov
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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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