Weather Alert in Texas
Dense Fog Advisory issued February 13 at 6:16PM CST until February 14 at 6:00AM CST by NWS Houston/Galveston TX
AREAS AFFECTED: Chambers; Inland Galveston; Coastal Galveston; Galveston Island; Bolivar Peninsula
DESCRIPTION: * WHAT...Visibility one quarter mile or less in dense fog. * WHERE...Bolivar Peninsula, Chambers, Coastal Galveston, Galveston Island, and Inland Galveston Counties. * WHEN...Until 6 AM CST Saturday. * IMPACTS...Low visibility could make driving conditions hazardous. * ADDITIONAL DETAILS...Visibility will continue to deteriorate as sea fog moves in from the adjacent coastal waters. Barrier islands are most at risk for persistent quarter mile visibility this evening. Some visibility improvements may occur during the pre-dawn hours of Saturday morning.
INSTRUCTION: If driving, slow down, use your headlights, and leave plenty of distance ahead of you.
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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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