Weather Alert in Texas
Special Weather Statement issued May 6 at 6:48AM CDT by NWS San Angelo TX
AREAS AFFECTED: Concho; Coleman; McCulloch
DESCRIPTION: At 647 AM CDT, Doppler radar was tracking a strong thunderstorm near Eden, moving east at 35 mph. HAZARD...Wind gusts of 50 to 55 mph and pea size hail. SOURCE...Radar indicated. IMPACT...Gusty winds could knock down tree limbs and blow around unsecured objects. Minor hail damage to vegetation is possible. Locations impacted include... Eden, Melvin, The Intersection Of Us-87 And Ranch Road 2134, Brady Lake, Fife, Live Oak, Us-83 Near The Menard-Concho County Line, Us-283 Near The Mcculloch-Coleman County Line, Lohn, Rochelle, Pear Valley, Doole, Stacy, Brady, Waldrip, The Intersection Of Us-83 And Ranch Road 765, Salt Gap, Placid, Mercury, and Millersview.
INSTRUCTION: If outdoors, consider seeking shelter inside a building. A Severe Thunderstorm Watch remains in effect until 1000 AM CDT for west central Texas.
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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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