Weather Alert in Virginia
Special Weather Statement issued March 23 at 4:07AM EDT by NWS Wakefield VA
AREAS AFFECTED: Fluvanna; Prince Edward; Cumberland; Goochland; Caroline; Mecklenburg; Lunenburg; Nottoway; Amelia; Powhatan; Brunswick; Dinwiddie; Western Louisa; Eastern Louisa; Western Hanover; Western Chesterfield; Eastern Chesterfield (Including Col. Heights); Western Henrico (Including the City of Richmond)
DESCRIPTION: * TIMING: From 1 PM Monday until 7 PM Monday evening. * WINDS...Northwest 10 to 15 mph with gusts to 20-25 mph. * RELATIVE HUMIDITY...As low as 25 to 30 percent. * TEMPERATURES...In the low to mid 70s. * IMPACTS...Low relative humidities and breezy northwest winds could produce favorable conditions for wildfires to ignite and spread today. Residents are urged to exercise caution handling any potential ignition source, including machinery, cigarettes, and matches. Be sure to properly discard all smoking materials. Any dry grasses and tree litter that ignite will have the potential to spread quickly. Virginia residents are reminded that open burning is prohibited before 4 PM each day through April 30th. The lowest relative humidity will come from mid to late afternoon on Monday, so any burning is highly discouraged.
INSTRUCTION: N/A
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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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