Weather Alert in Wisconsin
Flood Warning issued August 20 at 8:18PM CDT until August 21 at 7:00PM CDT by NWS La Crosse WI
AREAS AFFECTED: Buffalo, WI; Trempealeau, WI
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Wisconsin... Trempealeau River at Dodge affecting Trempealeau and Buffalo Counties. ...The Flood Warning continues for the following rivers in Iowa... Turkey River at Elkader affecting Clayton County. ...The Flood Warning is cancelled for the following rivers in Iowa... Cedar River at Charles City affecting Floyd County. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...Trempealeau River at Dodge. * WHEN...Until tomorrow evening. * IMPACTS...At 11.0 feet, The railroad bridge about three quarters of a mile upstream from the gage can restrict the flow. * ADDITIONAL DETAILS... - At 7:00 PM CDT Wednesday the stage was 10.8 feet. - Bankfull stage is 7.0 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 7:00 PM CDT Wednesday was 10.9 feet. - Forecast...The river is expected to fall below flood stage tomorrow morning and continue falling to 8.0 feet Wednesday, August 27. - Flood stage is 10.5 feet. - Flood History...This crest compares to a previous crest of 10.8 feet on 09/24/1986. - http://www.weather.gov/safety/flood
INSTRUCTION: Motorists should not attempt to drive around barricades or drive cars through flooded areas. Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional river and weather information is available at www.weather.gov/lacrosse. The next statement will be issued this evening by 930 PM CDT.
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Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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