Weather Alert in Maryland
Severe Thunderstorm Warning issued July 9 at 8:39PM EDT until July 9 at 9:15PM EDT by NWS Wakefield VA
AREAS AFFECTED: Somerset, MD; Worcester, MD; Accomack, VA
DESCRIPTION: At 839 PM EDT, a severe thunderstorm was located near Lawsonia, or 14 miles west 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 storm will be near... Marion Station around 845 PM EDT. Westover around 915 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.
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Weather Topic: What is Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
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