Weather Alert in Pennsylvania
Severe Thunderstorm Warning issued March 31 at 6:26PM EDT until March 31 at 8:00PM EDT by NWS Cleveland OH
AREAS AFFECTED: Crawford, PA; Erie, PA
DESCRIPTION: SVRCLE The National Weather Service in Cleveland has issued a * Severe Thunderstorm Warning for... Erie County in northwestern Pennsylvania... Crawford County in northwestern Pennsylvania... * Until 800 PM EDT. * At 626 PM EDT, severe thunderstorms were located along a line extending from 8 miles northwest of Girard to 8 miles northwest of Pymatuning North to near Kinsman, moving east at 50 mph. HAZARD...70 mph wind gusts and penny size hail. SOURCE...Radar indicated. IMPACT...Expect considerable tree damage. Damage is likely to mobile homes, roofs, and outbuildings. * Locations impacted include... Erie, Meadville, Conneaut, Corry, Edinboro, Titusville, North East, Union City, Girard, Cambridge Springs, Waterford, Albion, Linesville, Wattsburg, Adamsville, Pymatuning Central, Riceville, Harmonsburg, Guys Mills, and Pymatuning North.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building.
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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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