Weather Alert in Texas
Flood Watch issued May 5 at 11:38PM CDT until May 7 at 1:00AM CDT by NWS Houston/Galveston TX
AREAS AFFECTED: Houston; Trinity; Madison; Walker; San Jacinto; Polk; Brazos; Grimes
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall continues to be possible. * WHERE...A portion of southeast Texas, including the following counties, Brazos, Grimes, Houston, Madison, Polk, San Jacinto, Trinity and Walker. * WHEN...From 7 AM CDT Tuesday through late Tuesday night. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Flooding may occur in poor drainage and urban areas. * ADDITIONAL DETAILS... - A strong storm system will produce showers, heavy at times, and thunderstorms across the region on Tuesday. Rainfall totals of 1 to 3 inches can be broadly expected across SE Texas, though higher amounts of 3 to 6 inches will be possible in the watch area. Tuesday afternoon through Tuesday night will be the main timeframe to monitor for heavy rainfall over the current watch area, especially as some of these storms could become strong at times. Flood watch could be expanded further south heading into mid week depending on how conditions evolve. - http://www.weather.gov/safety/flood
INSTRUCTION: You should monitor later forecasts and be alert for possible Flood Warnings. Those living in areas prone to flooding should be prepared to take action should flooding develop.
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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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