Weather Alert in Texas
Flood Watch issued July 5 at 7:31PM CDT until July 6 at 7:00PM CDT by NWS San Angelo TX
AREAS AFFECTED: Coleman; Brown
DESCRIPTION: * WHAT...Flash flooding caused by excessive rainfall continues to be possible. * WHERE...A portion of west central Texas, including the following counties, Brown and Coleman. * WHEN...Through Sunday evening. * 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. Low-water crossings may be flooded. * ADDITIONAL DETAILS... - Scattered showers and thunderstorms are expected to increase in coverage across Brown and Coleman Counties overnight. Pockets of heavy rainfall will be possible, with some locations seeing totals of 3 to 5 inches late tonight into Sunday. A few locations may see even heavier totals. Although Brown and Coleman did not see the heaviest rainfall over the last week, this much rain on soils that are already saturated will still lead to flash flooding.
INSTRUCTION: You should monitor later forecasts and be prepared to take action should Flash Flood Warnings be issued. Flash flooding can be especially dangerous. Make sure you have a way of receiving warnings during the overnight hours.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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
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