Weather Alert in Kansas
Flood Warning issued February 15 at 7:39AM CST until February 15 at 3:40PM CST by NWS Topeka KS
AREAS AFFECTED: Anderson, KS
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Kansas... Cottonwood River near Emporia affecting Lyon County. ...The Flood Warning continues for the following rivers in Kansas... Pottawatomie Creek near Garnett affecting Anderson County. Neosho River Near Neosho Rapids affecting Lyon County. * WHAT...Minor flooding is occurring. * WHERE...Pottawatomie Creek near Garnett. * WHEN...Until late this afternoon. * IMPACTS...At 26.0 feet, Flood waters overflow the north bank and flood cultivated fields north of the creek. * ADDITIONAL DETAILS... - At 7:17 AM CST Sunday the stage was 26.3 feet. - Forecast...The river is expected to fall below flood stage late this morning and continue falling to 4.3 feet Friday morning. - Flood stage is 26.0 feet.
INSTRUCTION: Be especially cautious at night when it is harder to recognize the dangers of flooding. Caution is urged when walking near riverbanks. Motorists should not attempt to drive around barricades or drive cars through flooded areas. This product along with additional weather and stream information is available at www.weather.gov/top/.
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Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
Weather Topic: What is Graupel?
Home - Education - Precipitation - Graupel
Next Topic: Hail
Graupel is a form of precipitation that is created by atmospheric conditions
which cause supercooled water droplets to contact snow crystals and freeze to
their surface.
Sometimes known as soft hail or snow pellets, graupel is delicate and easily
destroyed by touch. Whereas hail usually falls during severe weather, graupel
doesn't require such conditions to form, and can form in mild precipitation
similar to situations which produce snowfall.
Next Topic: Hail
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