Weather Alert in Minnesota
Flood Warning issued August 13 at 10:37AM CDT until August 15 at 7:00PM CDT by NWS Grand Forks ND
AREAS AFFECTED: Clay, MN
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Minnesota... South Branch Buffalo River at Sabin affecting Clay County. ...The Flood Warning continues for the following rivers in Minnesota... Buffalo River near Dilworth affecting Clay County. * WHAT...Minor flooding is occurring and minor flooding is forecast. * WHERE...South Branch Buffalo River at Sabin. * WHEN...Until Friday evening. * IMPACTS...At 14.0 feet, Agricultural flooding begins. * ADDITIONAL DETAILS... - At 9:45 AM CDT Wednesday the stage was 13.9 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 9:45 AM CDT Wednesday was 14.3 feet. - Forecast...The river is expected to fall below flood stage tomorrow afternoon and continue falling. - Flood stage is 13.0 feet.
INSTRUCTION: Safety message - Turn around, don't drown. Don't travel through flooded areas. Most flood deaths occur in vehicles. Additional information is available at www.weather.gov.
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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
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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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