Weather Alert in Texas
Severe Thunderstorm Watch issued May 25 at 10:14PM CDT until May 26 at 1:00AM CDT by NWS Lubbock TX
AREAS AFFECTED: Briscoe, TX; Childress, TX; Cottle, TX; Crosby, TX; Dickens, TX; Floyd, TX; Garza, TX; Hale, TX; Hall, TX; Kent, TX; King, TX; Lubbock, TX; Lynn, TX; Motley, TX; Stonewall, TX; Swisher, TX
DESCRIPTION: THE NATIONAL WEATHER SERVICE HAS ISSUED SEVERE THUNDERSTORM WATCH 326 UNTIL 1 AM CDT MONDAY WHICH REPLACES A PORTION OF TORNADO WATCH 325. THE NEW WATCH IS VALID FOR THE FOLLOWING AREAS IN TEXAS THE NEW WATCH INCLUDES 16 COUNTIES IN NORTHWEST TEXAS COTTLE CROSBY DICKENS FLOYD GARZA HALE KENT KING LUBBOCK LYNN MOTLEY STONEWALL IN THE PANHANDLE OF TEXAS BRISCOE CHILDRESS HALL SWISHER THIS INCLUDES THE CITIES OF ASPERMONT, CEE VEE, CHILDRESS, CROSBYTON, DICKENS, DUMONT, FLOYDADA, GUTHRIE, HALE CENTER, HAPPY, JAYTON, KIRKLAND, LAKE ALAN HENRY, LOCKNEY, LUBBOCK, MATADOR, MEMPHIS, NEW HOME, ODONNELL, OLD GLORY, PADUCAH, PLAINVIEW, POST, QUITAQUE, RALLS, ROARING SPRINGS, SILVERTON, SLATON, SPUR, TAHOKA, TULIA, TURKEY, AND WOLFFORTH.
INSTRUCTION: N/A
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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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