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 is Sleet?
Home - Education - Precipitation - Sleet
Next Topic: Snow
Sleet is a form of precipitation in which small ice pellets are the primary
components. These ice pellets are smaller and more translucent than hailstones,
and harder than graupel. Sleet is caused by specific atmospheric conditions and
therefore typically doesn't last for extended periods of time.
The condition which leads to sleet formation requires a warmer body of air to be
wedged in between two sub-freezing bodies of air. When snow falls through a warmer
layer of air it melts, and as it falls through the next sub-freezing body of air
it freezes again, forming ice pellets known as sleet. In some cases, water
droplets don't have time to freeze before reaching the surface and the result is
freezing rain.
Next Topic: Snow
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
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