Weather Alert in Tennessee
Severe Thunderstorm Warning issued April 3 at 3:53AM CDT until April 3 at 4:30AM CDT by NWS Nashville TN
AREAS AFFECTED: Hickman, TN; Lewis, TN; Perry, TN; Wayne, TN
DESCRIPTION: SVROHX The National Weather Service in Nashville has issued a * Severe Thunderstorm Warning for... Western Lewis County in Middle Tennessee... Northern Wayne County in Middle Tennessee... Southern Perry County in Middle Tennessee... Southwestern Hickman County in Middle Tennessee... * Until 430 AM CDT. * At 353 AM CDT, a severe thunderstorm was located 10 miles north of Olive Hill, or 17 miles northeast of Savannah, moving east at 50 mph. HAZARD...60 mph wind gusts and quarter size hail. SOURCE...Radar indicated. IMPACT...Hail damage to vehicles is expected. Expect wind damage to roofs, siding, and trees. * Locations impacted include... Clifton, Flatwoods, Hohenwald, Linden, and Pleasantville.
INSTRUCTION: Remain alert for a possible tornado! Tornadoes can develop quickly from severe thunderstorms. If you spot a tornado go at once into the basement or small central room in a sturdy structure. For your protection move to an interior room on the lowest floor of a building. A Tornado Watch remains in effect until 600 AM CDT for Middle Tennessee.
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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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