Weather Alert in Indiana
Flood Warning issued March 3 at 12:35PM EST by NWS Indianapolis IN
AREAS AFFECTED: Jackson, IN; Lawrence, IN; Washington, IN
DESCRIPTION: ...The National Weather Service in Indianapolis IN has issued a Flood Warning for the following rivers in Indiana... East Fork White River at Seymour. White River at Elliston. White River at Newberry. .Multiple rounds of rainfall over central Indiana over the next several days are expected to bring at least minor flooding on area rivers and streams. Flooding is expected to develop along portions of the East Fork White and lower White basins over the next 48 hours. Forecast crests issued today include rainfall amounts of 3 to 4 inches over large portions of the East Fork White and lower White basins from this morning through Friday morning, but additional rainfall expected from Friday onward will likely increase crests and lengthen the amount of time in flood. * WHAT...Minor flooding is forecast. * WHERE...East Fork White River at Seymour. * WHEN...From Wednesday morning until further notice. * IMPACTS...At 16.4 feet, State Road 258 remained open after the river rebounded quickly to this level in June 2010. State Road 258 had been flooded a few days earlier after river crested at 17.9 feet. * ADDITIONAL DETAILS... - At 10:45 AM EST Tuesday the stage was 4.8 feet. - Forecast...The river will rise above flood stage late tomorrow morning to 15.8 feet Thursday morning and then to 16.4 feet early Friday afternoon. - Flood stage is 12.0 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 late tonight by around 345 AM EST.
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Weather Topic: What is Condensation?
Home - Education - Precipitation - Condensation
Next Topic: Contrails
Condensation is the process which creates clouds, and therefore
it is a crucial process in the water cycle.
Condensation is the change of matter from a state of gas into a state of liquid,
and it happens because water molecules release heat into the atmosphere and
become organized into a more closely packed structure, what we might see as
water droplets.
Water is always present in the air around us as a vapor, but it's too small for
us to see. When water undergoes the process of condensation it becomes organized
into visible water droplets. You've probably seen condensation happen before on the
surface of a cold drink!
Next Topic: Contrails
Weather Topic: What are Cumulonimbus Clouds?
Home - Education - Cloud Types - Cumulonimbus Clouds
Next Topic: Cumulus Clouds
The final form taken by a growing cumulus cloud is the
cumulonimbus cloud, which is very tall and dense.
The tower of a cumulonimbus cloud can soar 23 km into the atmosphere, although
most commonly they stop growing at an altitude of 6 km.
Even small cumulonimbus clouds appear very large in comparison to other cloud types.
They can signal the approach of stormy weather, such as thunderstorms or blizzards.
Next Topic: Cumulus Clouds
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