Weather Alert in Texas
Flood Watch issued April 25 at 2:08PM CDT until April 26 at 4:00AM CDT by NWS Amarillo TX
AREAS AFFECTED: Oldham; Potter; Carson; Deaf Smith; Randall; Armstrong; Donley; Collingsworth; Palo Duro Canyon
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall is possible. * WHERE...The southern Panhandle of Texas, including the following areas, Armstrong, Carson, Collingsworth, Deaf Smith, Donley, Oldham, Palo Duro Canyon, Potter and Randall. * WHEN...From 5 PM CDT this afternoon through late tonight. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Flooding may occur in poor drainage and urban areas. Low-water crossings may be flooded. * ADDITIONAL DETAILS... - Heavy rainfall rates from strong to severe storms as well as potential training thunderstorms may produce localized areas of flooding this afternoon into the overnight hours, especially for urban areas or locations that have received heavy rainfall in recent days. - http://www.weather.gov/safety/flood
INSTRUCTION: You should monitor later forecasts and be alert for possible Flood Warnings. Those living in areas prone to flooding should be prepared to take action should flooding develop.
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Weather Topic: What is Snow?
Home - Education - Precipitation - 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
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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