Weather Alert in Indiana
Flood Warning issued June 30 at 9:42PM EDT until July 3 at 5:00AM EDT by NWS Indianapolis IN
AREAS AFFECTED: Gibson, IN; Knox, IN
DESCRIPTION: ...The Flood Warning continues for the following river in Indiana... White River at Edwardsport to Hazleton. .Rainfall amounts of 2 to 6 inches of rain fell across the area and upstream over the weekend. This will produce minor flooding along the White River near Edwardsport and points downstream in the coming days. River flooding should begin tonight and end by midweek. There are chances for additional isolated showers through this evening. * WHAT...Minor flooding is forecast. * WHERE...White River at Hazleton. * WHEN...From Wednesday morning to early Thursday morning. * IMPACTS...At 16.0 feet, Flooding begins in lowest bottomlands and a few local roads. High water affects a few low oil fields. * ADDITIONAL DETAILS... - There is no current observed data. - Forecast...The river is expected to rise above flood stage late Wednesday morning to a crest of 16.2 feet early Wednesday afternoon. It will then fall below flood stage Wednesday afternoon. - Flood stage is 16.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at www.weather.gov/ind. The next statement should be issued Tuesday afternoon by around 1245 PM EDT /1145 AM CDT/.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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