Weather Alert in New Mexico
Hydrologic Outlook issued August 27 at 1:54PM 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 is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
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.
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