Weather Alert in Florida

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Current Alerts for Flagler Beach, FL: Rip Current Statement

Special Weather Statement issued August 21 at 5:27PM EDT by NWS Jacksonville FL

AREAS AFFECTED: Baker; Union; Southeastern Columbia

DESCRIPTION: At 526 PM EDT, Doppler radar was tracking a strong thunderstorm over Olustee, or 11 miles east of Lake City. A strong thunderstorm was nearly stationary. HAZARD...Wind gusts up to 50 mph, pea size hail, and excessive cloud- to-ground lightning, minor flooding due to heavy rainfall. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Minor hail damage to vegetation is possible. Excessive cloud-to-ground lightning is occurring. This storm will remain over mainly rural areas of southwestern Baker, north central Union and east central Columbia Counties.

INSTRUCTION: If outdoors, consider seeking shelter inside a building.

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Weather Topic: What are Altocumulus Clouds?

Home - Education - Cloud Types - Altocumulus Clouds

Altocumulus Clouds Next Topic: Altostratus Clouds

Similar to cirrocumulus clouds, altocumulus clouds are characterized by cloud patches. They are distinguished by larger cloudlets than cirrocumulus clouds but are still smaller than stratocumulus clouds.

Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km) and may resemble, at times, the shape of a flying saucer. These uncommon formations, called altocumulus lenticularis, are created by uplift in the atmosphere and are most often seen in close proximity to mountains.

Next Topic: Altostratus Clouds

Weather Topic: What are Cirrocumulus Clouds?

Home - Education - Cloud Types - Cirrocumulus Clouds

Cirrocumulus Clouds Next Topic: Cirrostratus Clouds

Cirrocumulus clouds form at high altitudes (usually around 5 km) and have distinguishing characteristics displayed in a fine layer of small cloud patches. These small cloud patches are sometimes referred to as "cloudlets" in relation to the whole cloud formation.

Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the water droplets in the cloud freeze into ice crystals and the cloud becomes a cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud formations generally pass rapidly.

Next Topic: Cirrostratus Clouds

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