Weather Alert in Florida
Special Weather Statement issued May 9 at 12:36PM EDT by NWS Tallahassee FL
AREAS AFFECTED: Inland Gulf; Inland Franklin; Inland Wakulla; Coastal Gulf; Coastal Franklin; Southern Liberty
DESCRIPTION: At 1235 PM EDT/1135 AM CDT/, Doppler radar was tracking strong thunderstorms along a line extending from 9 miles northeast of Port St. Joe to 11 miles northwest of Carrabelle. Movement was north at 10 mph. HAZARD...Wind gusts up to 40 mph and pea size hail. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Minor hail damage to vegetation is possible. Locations impacted include... East Camp, Honeyville, Buck Siding, Morgan Place, Stonemill Creek, High Bluff, Chipola Cutoff, Wewahitchka, Beverly, Owens Bridge, White City, Poplar Camp, Kern, Wilma, Sumatra, Howard Creek, Willis Landing, Twin Pole, Creels, and Hays Place.
INSTRUCTION: Torrential rainfall is also occurring with these storms and may lead to localized flooding. Do not drive your vehicle through flooded roadways. Frequent cloud to ground lightning is occurring with these storms. Lightning can strike 10 miles away from a thunderstorm. Seek a safe shelter inside a building or vehicle.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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
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