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 is Sleet?
Home - Education - Precipitation - Sleet
Next Topic: Snow
Sleet is a form of precipitation in which small ice pellets are the primary
components. These ice pellets are smaller and more translucent than hailstones,
and harder than graupel. Sleet is caused by specific atmospheric conditions and
therefore typically doesn't last for extended periods of time.
The condition which leads to sleet formation requires a warmer body of air to be
wedged in between two sub-freezing bodies of air. When snow falls through a warmer
layer of air it melts, and as it falls through the next sub-freezing body of air
it freezes again, forming ice pellets known as sleet. In some cases, water
droplets don't have time to freeze before reaching the surface and the result is
freezing rain.
Next Topic: Snow
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
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