Weather Alert in Florida
Special Weather Statement issued February 27 at 4:12AM EST by NWS Tampa Bay Ruskin FL
AREAS AFFECTED: Sumter; Polk; Hardee; Highlands; DeSoto; Coastal Citrus; Coastal Hernando; Coastal Pasco; Coastal Hillsborough; Coastal Manatee; Coastal Sarasota; Coastal Charlotte; Coastal Lee; Inland Citrus; Inland Hernando; Inland Pasco; Inland Hillsborough; Inland Manatee; Inland Sarasota; Inland Charlotte; Inland Lee
DESCRIPTION: At 411 AM EST, satellite imagery and surface observations indicate fog is reducing visibilities to 1/2 mile or less at times. Locations impacted include... Lecanto, Lake Manatee State Park, New Port Richey East, Shady Hills, Fort Myers Villas, South Gate Ridge, St. Leo, Sumterville, Bushnell, Lake Sarasota, Weeki Wachee, Placid Lakes, Haines City, Southwest Florida Airport, Winston, Floral City, Bradenton Beach, East Lake-Orient Park, Southgate, and Chassahowitzka Refuge. Motorists should be prepared for sudden changes in visibility. Use low beam headlights, reduce your speed, and maintain a safe distance between your vehicle and the one ahead of you.
INSTRUCTION: N/A
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
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
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