Weather Alert in New Mexico
High Wind Watch issued March 14 at 1:47AM MDT until March 15 at 6:00PM MDT by NWS Albuquerque NM
AREAS AFFECTED: Glorieta Mesa Including Glorieta Pass; Northern Sangre de Cristo Mountains; Southern Sangre de Cristo Mountains; East Slopes Sangre de Cristo Mountains; Santa Fe Metro Area; Middle Rio Grande Valley/Albuquerque Metro Area; Sandia/Manzano Mountains Including Edgewood; Estancia Valley; Central Highlands; South Central Highlands; South Central Mountains; Johnson and Bartlett Mesas Including Raton Pass; Far Northeast Highlands; Northeast Highlands; Union County; Harding County; Eastern San Miguel County; Guadalupe County; Quay County; Curry County; Roosevelt County; De Baca County; Chaves County Plains; Eastern Lincoln County; Southwest Chaves County
DESCRIPTION: * WHAT...Northwest winds 30 to 40 mph with gusts of 60 to 70 mph possible. * WHERE...Portions of central, east central, north central, northeast, and southeast New Mexico. * WHEN...From late tonight through Sunday afternoon. * IMPACTS...Damaging winds could blow down trees and power lines. Power outages are possible. Travel will be difficult, especially for high profile vehicles. * ADDITIONAL DETAILS...Localized areas of blowing dusts may reduce visibility.
INSTRUCTION: Monitor the latest forecasts and warnings for updates.
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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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