Weather Alert in Maryland
High Wind Watch issued February 5 at 1:03PM EST until February 7 at 10:00PM EST by NWS Wakefield VA
AREAS AFFECTED: Dorchester; Wicomico; Somerset; Inland Worcester; Maryland Beaches; Accomack; Northampton
DESCRIPTION: * WHAT...For the High Wind Watch, northwest winds 30 to 40 mph with gusts up to 55 mph possible. For the Extreme Cold Watch, dangerously cold wind chills as low as 10 below possible. * WHERE...In Maryland, Dorchester, Inland Worcester, Maryland Beaches, Somerset, and Wicomico Counties. In Virginia, Northampton and Accomack Counties. * WHEN...For the High Wind Watch, from Saturday morning through Saturday evening. For the Extreme Cold Watch, from Saturday evening through Sunday morning. * IMPACTS...Damaging winds could blow down trees and power lines. Scattered power outages are possible. Travel could be difficult, especially for high profile vehicles. The cold wind chills as low as 10 below zero could result in hypothermia if precautions are not taken.
INSTRUCTION: Monitor the latest forecasts and warnings for updates. Fasten loose objects or shelter objects in a safe location prior to the onset of winds. Dress in layers including a hat, face mask, and gloves if you must go outside. Keep pets indoors as much as possible. Make frequent checks on older family, friends, and neighbors. Ensure portable heaters are used correctly. Do not use generators or grills inside.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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