Weather Alert in New Mexico
Flood Warning issued May 8 at 3:33PM MDT until May 9 at 3:30PM MDT by NWS Albuquerque NM
AREAS AFFECTED: San Miguel, NM
DESCRIPTION: * WHAT...Flooding caused by rain and snowmelt is expected. * WHERE...A portion of northeast New Mexico, including the following county, northwestern San Miguel. * WHEN...Until 330 PM MDT Friday. * IMPACTS...Flooding of rivers, creeks, streams, and other low-lying and flood-prone locations is imminent or occurring. Expect many areas of slow moving or standing water. * ADDITIONAL DETAILS... - At 332 PM MDT, local law enforcement and the public reported heavy rain and snowmelt in the warned area due to thunderstorms. Flooding is already occurring. - This includes the following streams and drainages... Sparks Creek, Manuelitas Creek, San Jose, Rito, Maestas Creek and Sapello River. Additional rainfall amounts up to 0.25 inches are possible in the warned area. - Some locations that will experience flooding include... Rociada. - http://www.weather.gov/safety/flood
INSTRUCTION: Be especially cautious at night when it is harder to recognize the dangers of flooding. Stay away or be swept away. River banks and culverts can become unstable and unsafe.
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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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