Weather Alert in Indiana
Flood Advisory issued March 4 at 7:31AM EST until March 4 at 11:00AM EST by NWS Indianapolis IN
AREAS AFFECTED: Clay, IN; Morgan, IN; Owen, IN; Putnam, IN
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall continues. * WHERE...Morgan County in central Indiana... Northern Clay County in west central Indiana... Northeastern Owen County in west central Indiana... Southern Putnam County in west central Indiana... * WHEN...Until 1100 AM EST. * IMPACTS...Minor flooding in low-lying and poor drainage areas. River or stream flows are elevated. * ADDITIONAL DETAILS... - At 726 AM EST, Doppler radar indicated heavy rain due to thunderstorms overnight and stream gauges show elevated levels with some indicating minor flooding. Between 1.5 and 3 inches of rain have fallen. - Some locations that will experience flooding include... Martinsville, Mooresville, Brazil, Cloverdale, Brooklyn, Monrovia, Morgantown, Knightsville, Gosport, Paragon, Harmony, Carbon, Center Point, Bethany, Quincy, Devore, Eminence, Belle Union, Little Point and Cagles Mill Lake. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles.
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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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