Weather Alert in Maryland
Flood Watch issued June 27 at 3:27AM EDT until June 27 at 10:00PM EDT by NWS Baltimore MD/Washington DC
AREAS AFFECTED: Western Garrett; Eastern Garrett; Augusta; Rockingham; Western Highland; Eastern Highland; Hardy; Western Grant; Eastern Grant; Western Mineral; Western Pendleton; Eastern Pendleton
DESCRIPTION: * WHAT...Flash flooding caused by excessive rainfall is possible. * WHERE...Portions of western Maryland, including the following areas, Eastern Garrett and Western Garrett, western Virginia, including the following areas, Augusta, Eastern Highland, Rockingham and Western Highland, and eastern West Virginia, including the following areas, Eastern Grant, Eastern Pendleton, Hardy, Western Grant, Western Mineral and Western Pendleton. * WHEN...From 1 PM EDT this afternoon through this evening. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. * ADDITIONAL DETAILS... - Thunderstorms are expected to form this afternoon as a backdoor cold front runs into the higher terrain. Storms will produce very heavy rainfall and move very slowly. Rainfall amounts of 1 to 3 inches are possible, with isolated totals of 3 to 5 inches. Flash flooding may occur as a result. - Please visit www.weather.gov/safety/flood for flood safety and preparedness information
INSTRUCTION: You should monitor later forecasts and be prepared to take action should Flash Flood Warnings be issued.
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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