Weather Alert in New Mexico
Flood Watch issued August 30 at 12:53AM MDT until August 31 at 6:00AM MDT by NWS Albuquerque NM
AREAS AFFECTED: Curry County; Roosevelt County; De Baca County; Chaves County Plains; Eastern Lincoln County; Southwest Chaves County
DESCRIPTION: * WHAT...Flash flooding caused by excessive rainfall continues to be possible. * WHERE...Portions of central, east central, and southeast New Mexico, including the following areas, in central New Mexico, Eastern Lincoln County. In east central New Mexico, Curry County, De Baca County and Roosevelt County. In southeast New Mexico, Chaves County Plains and Southwest Chaves County. * WHEN...From noon MDT today 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. Extensive street flooding and flooding of creeks and rivers are possible. * ADDITIONAL DETAILS... - Above normal atmospheric moisture and impressive instability will combine to produce torrential rain producing storms Saturday afternoon and night. Rainfall rates in excess of 3 inches per hour are likely. This heavy rainfall will fall over already saturated grounds from Friday's heavy rainfall, increasing the flash flood threat. - http://www.weather.gov/safety/flood
INSTRUCTION: You should monitor later forecasts and be prepared to take action should Flash Flood Warnings be issued.
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
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