Weather Alert in Texas
Severe Thunderstorm Warning issued April 29 at 6:48PM CDT until April 29 at 7:45PM CDT by NWS San Angelo TX
AREAS AFFECTED: Haskell, TX; Throckmorton, TX
DESCRIPTION: SVRSJT The National Weather Service in San Angelo has issued a * Severe Thunderstorm Warning for... Northeastern Haskell County in west central Texas... Northern Throckmorton County in west central Texas... * Until 745 PM CDT. * At 648 PM CDT, a severe thunderstorm was located near Us-277 Near The Haskell-Knox County Line, or near Weinert, moving east at 35 mph. HAZARD...70 mph wind gusts and half dollar size hail. SOURCE...Radar indicated. IMPACT...Hail damage to vehicles is expected. Expect considerable tree damage. Wind damage is also likely to mobile homes, roofs, and outbuildings. * This severe thunderstorm will be near... Millers Creek Reservoir around 655 PM CDT. Elbert around 740 PM CDT. Other locations impacted by this severe thunderstorm include Us- 277 Near The Haskell-Knox County Line and Us- 183 Near The Throckmorton-Baylor County Line.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. A Tornado Watch remains in effect until 100 AM CDT for west central Texas.
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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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