Weather Alert in Indiana
Flood Warning issued June 7 at 5:43AM EDT until June 9 at 3:17AM 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... Wabash River at Lafayette. ...The Flood Warning continues for the following rivers in Indiana... White River at Edwardsport and Elliston ...The Flood Warning is cancelled for the following rivers in Indiana... White River at Newberry. .Rainfall amounts of two to four inches across central Indiana is producing minor flooding along area waterways in west-central Indiana. Additional rainfall of half an inch to an inch is possible through Sunday. Additional information is available at www.weather.gov/ind. The next statement should be issued this morning by around 645 AM EDT /545 AM CDT/. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...White River at Elliston. * WHEN...Until early Monday morning. * IMPACTS...At 20.0 feet, River Road north of CR 150 W in Greene County is flooded. Low agricultural fields flood. * ADDITIONAL DETAILS... - At 8:00 AM EDT Friday the stage was 19.0 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 8:00 AM EDT Friday was 19.0 feet. - Forecast...The river is expected to rise to a crest of 20.3 feet this morning. It will then fall below flood stage tomorrow afternoon. - Flood stage is 18.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: N/A
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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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