Weather Alert in Maryland
Severe Thunderstorm Warning issued July 9 at 8:09PM EDT until July 9 at 9:15PM EDT by NWS Wakefield VA
AREAS AFFECTED: Somerset, MD; Worcester, MD; Accomack, VA
DESCRIPTION: SVRAKQ The National Weather Service in Wakefield has issued a * Severe Thunderstorm Warning for... Somerset County in southeastern Maryland... Southwestern Worcester County in southeastern Maryland... Northern Accomack County in southeastern Virginia... * Until 915 PM EDT. * At 809 PM EDT, a severe thunderstorm was located near Lawsonia, or 20 miles southwest of Pocomoke City, moving northeast at 10 mph. HAZARD...60 mph wind gusts. SOURCE...Radar indicated. IMPACT...Expect damage to trees and powerlines. * This severe thunderstorm will be near... Lawsonia around 815 PM EDT. Marion Station around 845 PM EDT. Other locations impacted by this severe thunderstorm include Oriole, Byrdtown, Cokesbury, Fairmount, Upper Hill, Smith Island, Hopewell, Rehobeth, Kingston, and Shelltown.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. Please report severe weather by calling 757-899-2415, posting to the NWS Wakefield Facebook page, or using X @NWSWAKEFIELDVA.
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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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