Weather Alerts for New Mexico
1. High Wind Warning for: Central Highlands; Guadalupe County
2. High Wind Warning for: Southern Sangre de Cristo Mountains; East Slopes Sangre de Cristo Mountains; Northeast Highlands; Eastern San Miguel County
3. Red Flag Warning for: Central Highlands
4. Red Flag Warning for: Chaves County Plains; Eddy Plains; Lea; Gaines; Dawson; Borden; Andrews; Martin; Howard; Loving; Eastern Culberson County; Reeves County Plains; Davis Mountains; Davis Mountains Foothills
5. Red Flag Warning for: Northeast Highlands
6. Red Flag Warning for: Northeast Plains; East Central Plains
7. Red Flag Warning for: Northeast Plains; East Central Plains
8. Wind Advisory for: Glorieta Mesa Including Glorieta Pass; Sandia/Manzano Mountains Including Edgewood; Estancia Valley; South Central Mountains; Far Northeast Highlands; Harding County; Quay County; Curry County; Roosevelt County; De Baca County; Eastern Lincoln County; Southwest Chaves County
9. Wind Advisory for: West Slopes Sacramento Mountains Below 7500 Feet; Sacramento Mountains Above 7500 Feet; East Slopes Sacramento Mountains Below 7500 Feet
10. Winter Storm Warning for: Tusas Mountains Including Chama
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North America Water Vapor (Moisture)
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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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