Weather Alert in Texas
Flood Advisory issued September 7 at 10:13AM CDT until September 7 at 1:15PM CDT by NWS San Angelo TX
AREAS AFFECTED: Kimble, TX
DESCRIPTION: * WHAT...Arroyo and small stream flooding caused by excessive rainfall is expected. * WHERE...A portion of west central Texas, including the following county, Kimble. * WHEN...Until 115 PM CDT. * IMPACTS...Minor flooding in low-lying and poor drainage areas. * ADDITIONAL DETAILS... - At 1012 AM CDT, Doppler radar indicated heavy rain due to thunderstorms. This will cause arroyo and small stream flooding. Between 1 and 2 inches of rain have fallen. - Additional rainfall amounts of 0.5 to 1 inch are expected over the area. This additional rain will result in minor flooding. - Some locations that will experience flooding include... Junction, Segovia, Yates Crossing, South Llano River State Park, The Intersection Of I-10 And Us 290 and I-10 Near The Kimble-Kerr County Line. - This includes Interstate 10 between Mile Markers 453 and 477. This includes the following Low Water Crossings... Park Road 73 crossing South Llano River, RM 385 crossing Falls Prong, RM 385 crossing Perdenales River, FM 2169 crossing Johnson Fork Creek, James River crossing Little Devils River, County Road 430 crossing Johnson Fork, County Road 430 crossing Joy Creek, KC 451 crossing Johnson Fork, crossings along County Road 410 and Old Segovia Rd. crossing Johnson Fork. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles.
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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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