Weather Alert in Florida
Flood Advisory issued August 3 at 4:41PM EDT until August 3 at 5:30PM EDT by NWS Miami FL
AREAS AFFECTED: Collier, FL
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall continues. * WHERE...A portion of southwest Florida, including the following county, Collier. * WHEN...Until 530 PM EDT. * IMPACTS...Minor flooding in low-lying and poor drainage areas. * ADDITIONAL DETAILS... - At 440 PM EDT, Doppler radar indicated heavy rains have ended over the advisory area. however, rainfall amounts between 2 and 4 inches have fallen over the advisory area. This amount of rainfall will take sometime to drain away. Therefore, the Flood Advisory will remain in effect until 530 PM EDT this evening. - Flooding impacts will continue, but no additional rainfall is expected. - Some locations that will experience flooding include... Golden Gate Estates, Orangetree, West Toll Gate On Alligator Alley and Intersection I-75 And Everglades Blvd. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Be aware of your surroundings and do not drive on flooded roads. Please report observed flooding to local emergency services or law enforcement and request they pass this information to the National Weather Service when you can do so safely.
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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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