Weather Alert in Florida
Special Weather Statement issued July 15 at 3:39PM EDT by NWS Tallahassee FL
AREAS AFFECTED: Inland Bay; Inland Gulf; Inland Franklin; Coastal Bay; Coastal Gulf; Coastal Franklin
DESCRIPTION: At 339 PM EDT/239 PM CDT/, Doppler radar was tracking strong thunderstorms along a line extending from near Panama City to near Mexico Beach to 11 miles south of Port St. Joe to 6 miles northeast of Eastpoint. Movement was southwest at 35 mph. HAZARD...Wind gusts up to 40 mph. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Locations impacted include... Panama City, Lynn Haven, Callaway, Eastpoint, Apalachicola, St George Island, Port St. Joe, Springfield, Mexico Beach, Hiland Park, Tyndall Air Force Base, Franklin, Parker, Royal Bluff, Allanton, Dirego Park, St George Island St Pk, College Station, Cape San Blas, and Beverly.
INSTRUCTION: If outdoors, consider seeking shelter inside a building. 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 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
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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