Weather Alert in Indiana
Flood Warning issued March 4 at 10:54PM EST until March 11 at 4:43AM EDT by NWS Indianapolis IN
AREAS AFFECTED: Daviess, IN; Greene, IN; Knox, IN
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Indiana... White River below Eagle Valley Power Plant. White River at Spencer. White River at Elliston. White River at Newberry. White River at Petersburg. ...The Flood Warning continues for the following rivers in Indiana... White River at Edwardsport. Youngs Creek at Amity. .Between 2 and 4 inches of rain have fallen across central Indiana as of early Wednesday morning. Up to 2 inches have fallen in south-central Indiana. This has led creeks to rise above flood stage and rivers will follow in the coming days. Additional rain is in the forecast over the next several days. * WHAT...Moderate flooding is forecast. * WHERE...White River at Newberry. * WHEN...Until Wednesday, March 11. * IMPACTS...At 20.0 feet, County Road 550 W in Green County is impassable. * ADDITIONAL DETAILS... - At 10:30 PM EST Wednesday the stage was 12.7 feet. - Forecast...The river is expected to rise above flood stage late this evening to a crest of 20.0 feet Saturday morning. It will then fall below flood stage Tuesday afternoon. - Flood stage is 13.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. Additional information is available at www.weather.gov/ind. The next statement should be issued Thursday afternoon by around 200 PM EST /100 PM CST/.
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Weather Topic: What are Contrails?
Home - Education - Cloud Types - Contrails
Next Topic: Cumulonimbus Clouds
A contrail is an artificial cloud, created by the passing of an
aircraft.
Contrails form because water vapor in the exhaust of aircraft engines is suspended
in the air under certain temperatures and humidity conditions. These contrails
are called exhaust contrails.
Another type of contrail can form due to a temporary reduction in air pressure
moving over the plane's surface, causing condensation.
These are called aerodynamic contrails.
When you can see your breath on a cold day, it is also because of condensation.
The reason contrails last longer than the condensation from your breath is
because the water in contrails freezes into ice particles.
Next Topic: Cumulonimbus Clouds
Weather Topic: What are Cumulus Clouds?
Home - Education - Cloud Types - Cumulus Clouds
Next Topic: Drizzle
Cumulus clouds are fluffy and textured with rounded tops, and
may have flat bottoms. The border of a cumulus cloud
is clearly defined, and can have the appearance of cotton or cauliflower.
Cumulus clouds form at low altitudes (rarely above 2 km) but can grow very tall,
becoming cumulus congestus and possibly the even taller cumulonimbus clouds.
When cumulus clouds become taller, they have a greater chance of producing precipitation.
Next Topic: Drizzle
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