Weather Alert in Kansas
Flood Watch issued August 27 at 2:30PM CDT until August 28 at 1:00PM CDT by NWS Wichita KS
AREAS AFFECTED: Cowley; Chautauqua
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall continues to be possible. * WHERE...Portions of South Central and Southeast Kansas, including the following counties, in South Central Kansas, Cowley. In Southeast Kansas, Chautauqua. * WHEN...From 7 PM CDT this evening through Thursday afternoon. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Low-water crossings may be flooded. * ADDITIONAL DETAILS... - A narrow zone of very heavy rainfall is expected to develop overnight into early Thursday morning along a Salina-to- Chanute line. Rainfall totals around 2 to 5 inches are currently being forecast with locally higher amounts possible. Though it has been relatively dry over the past 2 to 3 weeks, this amount of rainfall in a short amount of time could cause areas of localized flooding across the watch area.
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. Be especially cautious at night when it is harder to recognize the dangers of flooding.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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
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