Weather Alert in New Mexico
Hydrologic Outlook issued August 27 at 10:52AM 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 Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
Weather Topic: What is Graupel?
Home - Education - Precipitation - Graupel
Next Topic: Hail
Graupel is a form of precipitation that is created by atmospheric conditions
which cause supercooled water droplets to contact snow crystals and freeze to
their surface.
Sometimes known as soft hail or snow pellets, graupel is delicate and easily
destroyed by touch. Whereas hail usually falls during severe weather, graupel
doesn't require such conditions to form, and can form in mild precipitation
similar to situations which produce snowfall.
Next Topic: Hail
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