Weather Alert in New Mexico
Red Flag Warning issued March 12 at 8:02PM MDT until March 13 at 8:00PM MDT by NWS Albuquerque NM
AREAS AFFECTED: Central Highlands
DESCRIPTION: ...RED FLAG WARNING FRIDAY FROM NOON UNTIL 8 PM FOR THE CENTRAL HIGHLANDS DUE TO STRONG WIND AND LOW HUMIDITY... ...FIRE WEATHER WATCH SATURDAY FROM NOON UNTIL 10 PM FOR WEST CENTRAL NM, NORTHERN NM, SANDIA AND MANZANO MOUNTAINS, AND CENTRAL HIGHLANDS DUE TO STRONG WIND AND LOW HUMIDITY... Lighter winds across the eastern plains and northeast highlands on Friday, but they will remain strong enough across the Central Highlands for another round of critical fire weather conditions during the afternoon and early evening hours. Critical fire weather conditions will then become more extreme and widespread this weekend as a sharp upper level trough crossing the northern and central Rockies steers a strong jetstream over New Mexico with a potent surface trough in the lee of the southern Rockies. * AREA AND TIMING...Central Highlands (Zone 125) Friday from noon until 8 PM, and Saturday from noon until 10 PM. * 20 FOOT WINDS...West northwest 25 to 35 mph with gusts up to 45 mph Friday. Higher wind gusts of up to 55 mph Saturday afternoon and evening. * RELATIVE HUMIDITY...Minimum values between 7 and 10 percent Friday and Saturday. * IMPACTS...Any fires that develop will likely spread rapidly. Outdoor burning is not recommended. On Saturday, any fires that develop will likely spread rapidly and will be hard to control. Long range spotting and extreme fire behavior will be possible. Outdoor burning is discouraged.
INSTRUCTION: Please advise the appropriate officials or fire crews in the field of this Red Flag Warning.
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Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
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
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