Weather Alert in Florida
Flood Warning issued August 25 at 9:45AM EDT by NWS Tampa Bay Ruskin FL
AREAS AFFECTED: Hillsborough, FL
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Florida... Little Manatee River At Wimauma at US 301 affecting Hillsborough County. * WHAT...Minor flooding is forecast. * WHERE...Little Manatee River at Wimauma at US 301. * WHEN...From Tuesday morning until further notice. * IMPACTS...At 13.0 feet, The canoe rental area floods. * ADDITIONAL DETAILS... - At 9:00 AM EDT Monday the stage was 9.0 feet. - Bankfull stage is 11.0 feet. - Forecast...The river is expected to rise above flood stage tomorrow morning and continue rising to a crest of 12.7 feet Wednesday morning. - Flood stage is 11.0 feet. - Flood History...This crest compares to a previous crest of 12.7 feet on 02/02/1972. - https://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Additional information is available at www.weather.gov. The next statement will be issued late tonight by 1245 AM EDT.
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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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