Weather Alert in Minnesota
Red Flag Warning issued March 28 at 11:18AM CDT until March 28 at 7:00PM CDT by NWS Twin Cities/Chanhassen MN
AREAS AFFECTED: Douglas; Todd; Morrison; Mille Lacs; Kanabec; Stevens; Pope; Stearns; Benton; Sherburne; Isanti; Chisago; Swift; Chippewa; Kandiyohi; Meeker; Wright; Hennepin; Anoka; Ramsey; Washington; Renville; McLeod; Sibley; Carver; Scott; Dakota; Nicollet; Le Sueur; Rice; Goodhue; Waseca; Steele; Freeborn
DESCRIPTION: ...CRITICAL FIRE WEATHER CONDITIONS THIS AFTERNOON... .The combination of warmer temperatures in the mid 50s to lower 60s, very low relative humidity values between 15 to 20 percent, southwest winds gusting to 35 to 45 mph, and dry fuels will lead to critical fire weather conditions across central and southern Minnesota this afternoon and early evening. * AFFECTED AREA...Portions of central, east central, south central, southeast, and west central Minnesota. * TIMING...Until 7 PM CDT this evening. * WINDS...Southwest winds 20 to 30 mph with gusts up to 40 mph. * RELATIVE HUMIDITY...As low as 19 percent. * IMPACTS...Any fires that develop will spread rapidly. Outdoor burning is not recommended.
INSTRUCTION: Please advise the appropriate officials or fire crews in the field of this Red Flag Warning.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
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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