Weather Alert in New Mexico

Recent Locations: Dunlo, PA   Questa, NM   Egg Harbor City, NJ  

Red Flag Warning issued February 16 at 1:49AM MST until February 17 at 7:00PM MST by NWS Albuquerque NM

AREAS AFFECTED: Northeast Highlands

DESCRIPTION: ...RED FLAG WARNING IN EFFECT FROM 11 AM TO 6 PM TODAY FOR THE NORTHEAST HIGHLANDS DUE TO STRONG WINDS AND LOW HUMIDITY... ...RED FLAG WARNING IN EFFECT FROM 10 AM TO 7 PM TUESDAY FOR THE NORTHEAST HIGHLANDS, NORTHEAST PLAINS, AND EAST-CENTRAL PLAINS DUE TO STRONG WINDS AND LOW HUMIDITY... .A storm system approaching from the west will allow southwest winds to increase today. This combined with relative humidity values in the low teens will result in critical fire weather conditions across parts of northeast NM this afternoon. Much stronger to damaging southwest to west winds will impact New Mexico Tuesday with critical fire weather over a larger area of eastern NM. Potential for peak wind gusts of 55 to 70 mph with minimum humidity values of 15 to 20% will allow for rapid fire spread among fine fuels. The National Weather Service in Albuquerque has issued a Red Flag Warning...which is in effect from 10 AM to 7 PM MST Tuesday. The Fire Weather Watch is no longer in effect. * AREA AND TIMING...Northeast Highlands (Zone 123) Monday and Tuesday. * 20 FOOT WINDS...For Monday afternoon, southwest 20 to 25 mph with gusts up to 40 mph. For Tuesday afternoon and evening, southwest to west 30 to 40 mph with peak gusts of 55 to 70 mph. * RELATIVE HUMIDITY...For Monday afternoon, minimum values of 10 to 15%. For Tuesday afternoon, minimum values of 15 to 20% * 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 Red Flag Warning.

View All Alerts for New Mexico

Want more detail? Get the Complete 7 Day and Night Detailed Forecast!

Want to Receive our Free Daily Forecast Emails in your inbox by 5 a.m.?
There are no ads! Learn More
We respect your privacy and will not share or sell your email with anyone.

Current U.S. National Radar--Current

The Current National Weather Radar is shown below with a UTC Time (subtract 5 hours from UTC to get Eastern Time).

Current U.S. National Radar

National Weather Forecast--Current

The Current National Weather Forecast and National Weather Map are shown below.

Today's National Weather Map

National Weather Forecast for Tomorrow

Tomorrow National Weather Forecast and Tomorrow National Weather Map are show below.

Tomorrows National Weather Map

North America Water Vapor (Moisture)

This map shows recent moisture content over North America. Bright and colored areas show high moisture (ie, clouds); brown indicates very little moisture present; black indicates no moisture.

North American Water Vapor Map

Weather Topic: What is Precipitation?

Home - Education - Precipitation - 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

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

Current conditions powered by WeatherAPI.com