Weather Alert in Kansas
Flood Watch issued August 24 at 1:44PM CDT until August 25 at 10:00AM CDT by NWS Dodge City KS
AREAS AFFECTED: Lane; Ness; Rush; Hodgeman; Pawnee; Stafford; Ford; Edwards; Kiowa; Pratt; Comanche; Barber
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is possible. * WHERE...Portions of central, south central, southwest, and west central Kansas, including the following counties, in central Kansas, Rush. In south central Kansas, Barber, Comanche, Edwards, Kiowa, Pawnee, Pratt and Stafford. In southwest Kansas, Ford and Hodgeman. In west central Kansas, Lane and Ness. * WHEN...From 10 PM CDT this evening through Monday morning. * IMPACTS...Extensive street flooding and flooding of creeks and rivers are possible. * ADDITIONAL DETAILS... - One to three inches of rainfall has already fallen, and and additional rainfall Tonight may cause scattered flash flooding. - http://www.weather.gov/safety/flood
INSTRUCTION: You should monitor later forecasts and be alert for possible Flood Warnings. Those living in areas prone to flooding should be prepared to take action should flooding develop.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
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
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