Weather Alert in Indiana
Winter Weather Advisory issued February 22 at 9:04PM EST until February 23 at 1:00PM EST by NWS Northern Indiana
AREAS AFFECTED: Starke; Marshall; Northern La Porte; Eastern St. Joseph; Southern La Porte; Western St. Joseph; Cass; Northern Berrien; Southern Berrien
DESCRIPTION: * WHAT...Lake effect snow. Additional snow accumulations between 2 and 4 inches. Local amounts up to 6 inches are possible. * WHERE...Portions of northern Indiana and southwest Michigan. * WHEN...Until 1 PM EST /noon CST/ Monday. * IMPACTS...Plan on slippery road conditions. The hazardous conditions will impact the Monday morning commute. * ADDITIONAL DETAILS...Winds gusting to around 25 mph. Blowing and drifting of snowfall will be possible.
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 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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