Weather Alert in North Carolina
Beach Hazards Statement issued July 5 at 11:28AM EDT until July 5 at 8:00PM EDT by NWS Wilmington NC
AREAS AFFECTED: Coastal Brunswick
DESCRIPTION: * WHAT...For the Beach Hazards Statement, Strong east to west longshore current. There is also a Moderate Risk of rip currents. For the High Surf Advisory, large breaking waves of 4 to 7 feet expected in the surf zone. * WHERE...Coastal Brunswick County. * WHEN...For the Beach Hazards Statement, until 8 PM EDT this evening. For the High Surf Advisory, from 6 AM to 8 PM EDT Sunday. * IMPACTS...Dangerous swimming and surfing conditions and localized beach erosion. Longshore currents can sweep swimmers and surfers into rip currents, piers, jetties, and other hazardous areas. It may sweep swimmers off their feet, making it difficult to return to shore.
INSTRUCTION: Inexperienced swimmers should remain out of the water due to dangerous surf conditions. Caution should be used when in or near the water. Check with lifeguards before entering the ocean for possible hazards you may be swept into.
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - 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
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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