Weather Alert in New Mexico
Flood Warning issued May 8 at 3:30PM MDT until May 9 at 3:30PM MDT by NWS Albuquerque NM
AREAS AFFECTED: Mora, NM
DESCRIPTION: * WHAT...Flooding caused by rain and snowmelt is occurring. * WHERE...A portion of northeast New Mexico, including the following county, southwestern Mora. * 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 329 PM MDT, local law enforcement and the public reported flooding in the warned area. Flooding is already occurring. - This includes the following streams and drainages... Cebolla, Rito, Casa, Rio la, Canada de los Maes, La, Sparks Creek, San Jose, Rito, Caoncito Creek and Mora River. Additional rainfall amounts up to 0.25 inches are possible in the warned area. - Some locations that will experience flooding include... Mora, Morphy Lake State Park, Ledoux, Cleveland, Gascon, Holman, Monte Aplanado and South Carmen. - 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 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
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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