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 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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