Weather Alert in New Mexico
Fire Weather Watch issued March 13 at 12:22PM MDT until March 15 at 8:00PM MDT by NWS Albuquerque NM
AREAS AFFECTED: Northwest Plateau; West Central Mountains; West Central Basin and Range; North Central Mountains; Upper Rio Grande Valley and Lower Chama River Valley; Sangre de Cristo Mountains; Sandia and Manzano Mountains
DESCRIPTION: ...RED FLAG WARNING TODAY UNTIL 8 PM FOR THE CENTRAL HIGHLANDS DUE TO STRONG WINDS AND LOW HUMIDITY... ...RED FLAG WARNING SATURDAY FROM NOON UNTIL MIDNIGHT FOR THE NORTHEAST HIGHLANDS, NORTHEAST PLAINS, AND CENTRAL HIGHLANDS DUE TO STRONG WINDS AND LOW HUMIDITY... ...FIRE WEATHER WATCH SATURDAY FROM 3 PM UNTIL 8 PM FOR WESTERN NM, NORTH CENTRAL NM AND THE SANDIA AND MANZANO MOUNTAINS DUE TO STRONG WINDS AND LOW HUMIDITY... ...FIRE WEATHER WATCH SUNDAY FOR ALL OF NORTHERN AND CENTRAL NM FROM 9 AM THROUGH 8 PM DUE TO STRONG WINDS AND LOW HUMIDITY... .Critical fire weather conditions will impact much of central and northern NM through the weekend. Critical fire weather conditions will persist across the Central Highlands today where gusty northwest winds have already developed. On Saturday, westerly winds will increase areawide, but will start earlier and linger longer across eastern NM. Therefore, long duration critical fire weather conditions are expected across much of eastern NM on Saturday, while a more focused period of critical fire weather conditions are possible from mid afternoon through early evening elsewhere. Very strong to damaging winds will develop early on Sunday and persist through the afternoon as both a Pacific and backdoor cold front press through the area. With gusts between 50 and 70 mph and single digit humidity values in many areas, critical to extreme fire weather conditions are likely despite cooling temperatures. The National Weather Service in Albuquerque has issued a Fire Weather Watch...which is in effect from Sunday morning through Sunday evening. * AREA AND TIMING...Northwest Plateau (Zone 101), West Central Mountains (Zone 105), West Central Basin and Range (Zone 109), North Central Mountains (Zone 120), Upper Rio Grande Valley and Lower Chama River Valley (Zone 121), Sangre de Cristo Mountains (Zone 122), and Sandia and Manzano Mountains (Zone 124) on Saturday from 3 PM until 8 PM and again Sunday from 9 AM through 8 PM. * 20 FOOT WINDS...On Saturday, west winds 20 to 30 mph with gusts up to 40 mph. The strongest winds will be during the evening. On Sunday, northwest winds 25 to 40 mph with gusts between 45 and 55 mph. * RELATIVE HUMIDITY...Minimum values between 6 and 15 percent with locally higher values across the peaks of the Tusas Mountains and Sangre de Cristo Mountains each day. * IMPACTS...Any fires that develop will likely spread rapidly. Outdoor burning is not recommended.
INSTRUCTION: Please advise the appropriate officials or fire crews in the field of this Fire Weather Watch.
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Weather Topic: What is Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
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
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