Weather Alert in New Mexico
Hydrologic Outlook issued August 28 at 9:06AM MDT by NWS Albuquerque NM
AREAS AFFECTED: Colfax, NM; Mora, NM; San Miguel, NM; Taos, NM
DESCRIPTION: ESFABQ Heightened Risk of River and Stream Flooding During Storm Events Through the Holiday Weekend. Repeated rounds of heavy rainfall in the area over the last several days have saturated the soils and raised the baseflow of rivers and streams in the area. We have reports of streams near the Mora, Sapello, Pecos and Vermejo river rising out of their banks, with additional reports of flowing water and debris across roads such as 518. These waterways will be extremely vulnerable to further rounds of precipitation, which we are expecting over the next week as a surge of deep monsoon moisture moves through the area. Expect further rises and impacts to nearby roads and low water crossings. Stay aware of any flash flood or river flood warnings that are issued. Exercise caution along riverbanks and watch out for potential mudslides across roads. For questions or comments about this outlook, you can contact Andrew Mangham, Senior Service Hydrologist, at 505-244-9150 x 228 or via e- mail at andrew.mangham@noaa.gov.
INSTRUCTION: N/A
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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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