Weather Alert in Indiana
Flood Warning issued June 30 at 9:42PM EDT until July 2 at 4:24AM EDT by NWS Indianapolis IN
AREAS AFFECTED: Daviess, IN; Gibson, IN; Knox, IN; Pike, 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 Edwardsport. * WHEN...From late tonight to early Wednesday morning. * IMPACTS...At 15.0 feet, Flooding of low agricultural fields begin. Daviess CR 375 WN and North River Rd in Knox County located inside the levees are flooded. * ADDITIONAL DETAILS... - At 7:00 PM EDT Monday /6:00 PM CDT Monday/ the stage was 14.0 feet. - Forecast...The river is expected to rise above flood stage late tonight to a crest of 15.3 feet tomorrow morning. It will then fall below flood stage tomorrow afternoon. - Flood stage is 15.0 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 are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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