Weather Alert in Texas
Severe Thunderstorm Warning issued June 10 at 2:10AM CDT until June 10 at 3:00AM CDT by NWS Midland/Odessa TX
AREAS AFFECTED: Ector, TX; Loving, TX; Reeves, TX; Ward, TX; Winkler, TX
DESCRIPTION: At 209 AM CDT, severe thunderstorms were located along a line extending from 12 miles southeast of Jal Airport to near Kermit to near Mentone, moving southeast at 25 mph. HAZARD...60 mph wind gusts and quarter size hail. SOURCE...Radar indicated. IMPACT...Hail damage to vehicles is expected. Expect wind damage to roofs, siding, and trees. Locations impacted include... Pecos, Monahans, Kermit, Wink, Mentone, Thorntonville, Barstow, Pyote, Wickett, Pecos Municipal Airport, Roy Hurd Memorial Airport, Monahans Sandhills State Park, Notrees, and Winkler County Airport. This includes Interstate 20 between mile markers 39 and 80, between mile markers 83 and 88, and between mile markers 91 and 97.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building. Torrential rainfall is occurring with these storms, and may lead to flash flooding. Do not drive your vehicle through flooded roadways.
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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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