Weather Alert in Texas
Flood Warning issued April 25 at 9:20PM CDT by NWS Shreveport LA
AREAS AFFECTED: Angelina, TX; Nacogdoches, TX
DESCRIPTION: ...The Flood Warning continues 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 occurring and minor flooding is forecast. * WHERE...Angelina River near Lufkin. * WHEN...Until further notice. * IMPACTS...At 161.0 feet, Expect minor flooding with the gravel parking lot flooded and water beginning to overflow the gravel road where it widens into the parking lot. Also expect about a foot of overflow across the left bank of the Angelina River looking downstream. * ADDITIONAL DETAILS... - At 8:45 PM CDT Friday the stage was 161.3 feet. - Bankfull stage is 158.5 feet. - Recent Activity...The maximum river stage in the 24 hours ending at 8:45 PM CDT Friday was 161.3 feet. - Forecast...The river is expected to rise to a crest of 161.5 feet tomorrow morning. - Flood stage is 161.0 feet. - Flood History...No available flood history. - 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 Saturday evening at 930 PM CDT.
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Weather Topic: What is Condensation?
Home - Education - Precipitation - Condensation
Next Topic: Contrails
Condensation is the process which creates clouds, and therefore
it is a crucial process in the water cycle.
Condensation is the change of matter from a state of gas into a state of liquid,
and it happens because water molecules release heat into the atmosphere and
become organized into a more closely packed structure, what we might see as
water droplets.
Water is always present in the air around us as a vapor, but it's too small for
us to see. When water undergoes the process of condensation it becomes organized
into visible water droplets. You've probably seen condensation happen before on the
surface of a cold drink!
Next Topic: Contrails
Weather Topic: What are Cumulonimbus Clouds?
Home - Education - Cloud Types - Cumulonimbus Clouds
Next Topic: Cumulus Clouds
The final form taken by a growing cumulus cloud is the
cumulonimbus cloud, which is very tall and dense.
The tower of a cumulonimbus cloud can soar 23 km into the atmosphere, although
most commonly they stop growing at an altitude of 6 km.
Even small cumulonimbus clouds appear very large in comparison to other cloud types.
They can signal the approach of stormy weather, such as thunderstorms or blizzards.
Next Topic: Cumulus Clouds
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