Weather Alert in Texas
Fire Warning issued February 17 at 10:44PM CST by NWS Amarillo TX
AREAS AFFECTED: Potter
DESCRIPTION: FRWAMA THE NATIONAL WEATHER SERVICE IN AMARILLO HAS ISSUED A FIRE WARNING AT THE REQUEST OF AMARILLO AREA OFFICE OF EMERGENCY MANAGEMENT FOR POTTER COUNTY. * AT 1042 PM CST...A DANGEROUS WILDFIRE WAS LOCATED 5 MILES EAST OF VALLEY DE ORO...OR 19 MILES NORTHWEST OF AMARILLO...MOVING EAST AT 2 TO 3 MPH. * AREAS IMPACTED... AREAS INBETWEEN TASCOSA ROAD AND US-287... INCLUDING THE US-287 CORRIDOR IN NORTH CENTRAL POTTER COUNTY. * ADDITIONAL INFORMATION...SMOKE AND FIRE WILL PRESENT A THREAT TO LIFE AND PROPERTY.
INSTRUCTION: BE PREPARED TO EVACUATE QUICKLY IF REQUESTED AND FOLLOW ALL SAFETY INSTRUCTIONS FROM LOCAL EMERGENCY MANAGEMENT OFFICIALS. DO NOT DRIVE INTO SMOKE.
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Weather Topic: What is Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
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