Weather Alert in Wisconsin
Flood Watch issued April 3 at 11:33PM CDT until April 8 at 7:00AM CDT by NWS La Crosse WI
AREAS AFFECTED: Crawford
DESCRIPTION: ...The National Weather Service in La Crosse WI has issued a Flood Watch for the following rivers in Wisconsin... Kickapoo River at Gays Mills affecting Crawford County. Yellow River at Necedah affecting Juneau County. .Heavy rain upstream of Gays Mills may cause the river gage to reach Minor flood stage early Monday morning. Additional heavy rain along the Yellow River may cause the Necedah gage to reach Minor flood stage early Monday morning. * WHAT...Flooding is possible. * WHERE...Kickapoo River at Gays Mills. * WHEN...From Monday morning to Wednesday morning. * IMPACTS...At 13.0 feet, Water begins to cover roads near the river, including Sand Hill Road near Bell Center. Minor flooding occurs in areas adjacent to the river, including Robb Park in Gays Mills. * ADDITIONAL DETAILS... - There is no current observed data. - Forecast...Flood stage may be reached Monday morning. - Flood stage is 13.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: If you are in the watch area, remain alert to possible flooding. Additional river and weather information is available at www.weather.gov/lacrosse. The next statement will be issued Saturday afternoon by 300 PM CDT.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
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Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
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
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