Weather Alert in Maryland
Special Weather Statement issued April 1 at 7:50PM EDT by NWS Wakefield VA
AREAS AFFECTED: Dorchester
DESCRIPTION: At 750 PM EDT, Doppler radar was tracking strong thunderstorms along a line extending from 10 miles east of Breezy Point to near Taylors Island to near Hollywood. Movement was east at 25 mph. HAZARD...Wind gusts up to 50 mph and pea size hail. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down small trees and blow around unsecured objects. Wind impacting handling of high profile vehicles. Minor hail damage to vegetation is possible. Strong thunderstorms will be near... Taylors Island around 755 PM EDT. Cambridge and University Of Maryland Center For Environmental Studies around 810 PM EDT. Other locations impacted by these storms include Madison, Brookview, Eldorado, Andrews, Hoopersville, Hudson, Honga, Church Creek, Wingate, and Lloyds.
INSTRUCTION: If outdoors, consider seeking shelter inside a building. These storms may intensify, so be certain to monitor local radio stations and available television stations for additional information and possible warnings from the National Weather Service.
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Weather Topic: What are Contrails?
Home - Education - Cloud Types - Contrails
Next Topic: Cumulonimbus Clouds
A contrail is an artificial cloud, created by the passing of an
aircraft.
Contrails form because water vapor in the exhaust of aircraft engines is suspended
in the air under certain temperatures and humidity conditions. These contrails
are called exhaust contrails.
Another type of contrail can form due to a temporary reduction in air pressure
moving over the plane's surface, causing condensation.
These are called aerodynamic contrails.
When you can see your breath on a cold day, it is also because of condensation.
The reason contrails last longer than the condensation from your breath is
because the water in contrails freezes into ice particles.
Next Topic: Cumulonimbus Clouds
Weather Topic: What are Cumulus Clouds?
Home - Education - Cloud Types - Cumulus Clouds
Next Topic: Drizzle
Cumulus clouds are fluffy and textured with rounded tops, and
may have flat bottoms. The border of a cumulus cloud
is clearly defined, and can have the appearance of cotton or cauliflower.
Cumulus clouds form at low altitudes (rarely above 2 km) but can grow very tall,
becoming cumulus congestus and possibly the even taller cumulonimbus clouds.
When cumulus clouds become taller, they have a greater chance of producing precipitation.
Next Topic: Drizzle
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