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 is Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
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