Weather Alert in Indiana
Flood Watch issued March 4 at 11:22AM EST until March 5 at 1:00PM EST by NWS Wilmington OH
AREAS AFFECTED: Wayne; Fayette; Union; Franklin; Ripley; Dearborn; Ohio; Switzerland; Carroll; Gallatin; Boone; Kenton; Campbell; Preble; Montgomery; Greene; Fayette; Pickaway; Butler; Warren; Clinton; Ross; Hocking; Hamilton; Clermont; Brown; Highland; Pike
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall continues to be possible. * WHERE...The following counties, in Indiana, Dearborn, Fayette, Franklin, Ohio, Ripley, Switzerland, Union and Wayne, the following counties, in northern Kentucky, Boone, Campbell, Carroll, Gallatin and Kenton, and the following counties, in Ohio, Brown, Butler, Clermont, Clinton, Fayette, Greene, Hamilton, Highland, Hocking, Montgomery, Pickaway, Pike, Preble, Ross and Warren. * WHEN...Through Thursday afternoon. * IMPACTS...Soils remain moist and excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. * ADDITIONAL DETAILS... - While there has been in a lull in rainfall, showers and some thunderstorms will move back into the region later this afternoon and continue into tonight and Thursday morning. Additional rainfall of 1 to 2 inches with locally higher amounts is possible. With much of the area saturated from rainfall over the past day, this additional rain may quickly result in flooding.
INSTRUCTION: You should monitor later forecasts and be alert for possible Flood Warnings. Those living in areas prone to flooding should be prepared to take action should flooding develop.
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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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