Weather Alert in New Mexico
Flood Watch issued June 30 at 2:06PM CDT until July 1 at 1:00AM CDT by NWS Midland/Odessa TX
AREAS AFFECTED: Guadalupe Mountains of Eddy County; Eddy County Plains; Northern Lea County; Central Lea County; Southern Lea County; Gaines; Dawson; Andrews; Loving; Winkler; Ector; Ward; Guadalupe Mountains Above 7000 Feet; Guadalupe and Delaware Mountains; Van Horn and Highway 54 Corridor; Eastern Culberson County; Reeves County Plains; Chinati Mountains; Marfa Plateau; Davis Mountains; Davis Mountains Foothills; Central Brewster County; Presidio Valley; Lower Brewster County
DESCRIPTION: * WHAT...Flash flooding caused by excessive rainfall continues to be possible. * WHERE...Portions of southeast New Mexico, including the following areas, Central Lea, Eddy County Plains, Guadalupe Mountains of Eddy County, Northern Lea and Southern Lea and Texas, including the following areas, Andrews, Central Brewster, Chinati Mountains, Davis Mountains, Davis Mountains Foothills, Dawson, Eastern Culberson, Ector, Gaines, Guadalupe Mountains Above 7000 Feet, Guadalupe and Delaware Mountains, Loving, Lower Brewster County, Marfa Plateau, Presidio Valley, Reeves County Plains, Van Horn and Highway 54 Corridor, Ward and Winkler. * WHEN...Until midnight MDT /1 AM CDT/ 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. * ADDITIONAL DETAILS... - 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 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
Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
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