Weather Alert in Florida

Recent Locations: Saint Maurice, LA   Henagar, AL   Dunnellon, FL  

Special Weather Statement issued February 25 at 10:11PM EST by NWS Miami FL

AREAS AFFECTED: Inland Collier County

DESCRIPTION: Dense smoke from the actively burning National Fire in Big Cypress National Preserve has resulted in reduced visibilities, less than 1 mile at times. The Florida Highway Patrol is currently in the process of closing Alligator Alley between SR-29 (Exit 80) and US-27 (Exit 23). Seek alternative routes and visit FL511 for additional road closure information. Reduced visibilities will remain possible through daybreak as smoke remains concentrated near the surface. Motorists are advised to drive with caution over the next several hours as visibilities may widely vary over short distances. Use low beam headlights and leave extra distance between your vehicle and others on the road when encountering significant reductions in visibility. Allow extra time to travel to destinations.

INSTRUCTION: N/A

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Weather Topic: What is Precipitation?

Home - Education - Precipitation - 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

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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