Weather Alert in Texas
Flood Warning issued April 24 at 10:22PM CDT by NWS Shreveport LA
AREAS AFFECTED: Angelina, TX; Nacogdoches, TX
DESCRIPTION: ...The Flood Warning is extended for the following rivers in Texas... Angelina River Near Lufkin affecting Angelina and Nacogdoches Counties. For the Angelina River...including Alto, Lufkin...Minor flooding is forecast. * WHAT...Minor flooding is forecast. * WHERE...Angelina River near Lufkin. * WHEN...From late tonight until further notice. * IMPACTS...At 162.0 feet, Minor lowland to diminish and end on the lower Angelina River. * ADDITIONAL DETAILS... - At 9:45 PM CDT Thursday the stage was 160.7 feet. - Bankfull stage is 158.5 feet. - Forecast...The river is expected to rise above flood stage late tonight and continue rising to a crest of 161.6 feet Saturday morning. - Flood stage is 161.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: Do not drive cars through flooded areas. Caution is urged when walking near riverbanks. Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Motorists should not attempt to drive around barricades or drive cars through flooded areas. For more hydrologic information, copy and paste the following website address into your favorite web browser URL bar: https://water.noaa.gov/wfo/SHV The next statement will be issued Friday evening at 1030 PM CDT.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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