Weather Alert in Indiana
Special Weather Statement issued February 23 at 4:11AM CST by NWS Chicago IL
AREAS AFFECTED: Lake; Jasper
DESCRIPTION: Lake-effect snow showers will persist across northwest Indiana this morning through this afternoon. Coverage and intensity of snow showers will increase this morning and early this afternoon, with additional accumulations of 1 to 2 inches possible especially across eastern Lake and northeastern Jasper counties. Gusty northwest winds will produce blowing and drifting of snow in open areas. Untreated roads will likely be snow covered and slippery, making for hazardous travel conditions. Snow showers should diminish this afternoon.
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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