Weather Alert in Texas

Recent Locations: Uvalde, TX  

Severe Thunderstorm Warning issued July 11 at 10:45PM CDT until July 11 at 11:30PM CDT by NWS Amarillo TX

AREAS AFFECTED: Deaf Smith, TX; Oldham, TX; Potter, TX

DESCRIPTION: SVRAMA The National Weather Service in Amarillo has issued a * Severe Thunderstorm Warning for... Oldham County in the Panhandle of Texas... Northern Deaf Smith County in the Panhandle of Texas... West central Potter County in the Panhandle of Texas... * Until 1130 PM CDT. * At 1045 PM CDT, severe thunderstorms were located along a line extending from 14 miles southwest of Channing to 4 miles west of Adrian to near Glenrio, moving southeast at 30 mph. HAZARD...60 mph wind gusts and penny size hail. SOURCE...Radar indicated. IMPACT...Minor damage to roofs, siding, and trees is possible. * Locations impacted include... Vega, Adrian, Glenrio, Valley De Oro, Boys Ranch, Wildorado, and Simms.

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 Snow?

Home - Education - Precipitation - Snow

Snow Next Topic: Stratocumulus Clouds

Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake, has unique characteristics, but all of them grow in a hexagonal structure. Snowfall can last for sustained periods of time and result in significant buildup of snow on the ground.

On the earth's surface, snow starts out light and powdery, but as it begins to melt it tends to become more granular, producing small bits of ice which have the consistency of sand. After several cycles of melting and freezing, snow can become very dense and ice-like, commonly known as snow pack.

Next Topic: Stratocumulus Clouds

Weather Topic: What are Stratus Clouds?

Home - Education - Cloud Types - Stratus Clouds

Stratus Clouds Next Topic: Wall Clouds

Stratus clouds are similar to altostratus clouds, but form at a lower altitude and are identified by their fog-like appearance, lacking the distinguishing features of most clouds.

Stratus clouds are wider than most clouds, and their base has a smooth, uniform look which is lighter in color than a nimbostratus cloud. The presence of a stratus cloud indicates the possibility of minor precipitation, such as drizzle, but heavier precipitation does not typically arrive in the form of a stratus cloud.

Next Topic: Wall Clouds

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