Weather Alert in New Mexico

Recent Locations: Fairbanks, AK   Hueysville, KY   Rio Rancho, NM  

Red Flag Warning issued February 17 at 5:34AM CST until February 17 at 8:00PM CST by NWS Midland/Odessa TX

AREAS AFFECTED: Chaves County Plains; Eddy Plains; Lea; Gaines; Loving; Van Horn and Highway 54 Corridor; Eastern Culberson County; Reeves County Plains; Chinati Mountains; Marfa Plateau; Davis Mountains; Davis Mountains Foothills

DESCRIPTION: ...RED FLAG WARNING IN EFFECT FROM 11 AM CST /10 AM MST/ TO 8 PM CST /7 PM MST/ TUESDAY FOR 20 FOOT WINDS OF 20 MPH OR GREATER, RELATIVE HUMIDITY AS LOW AS 15 PERCENT, AND HIGH FIRE DANGER ACROSS GAINES COUNTY, THE SOUTHEAST NEW MEXICO PLAINS, UPPER TRANS PECOS, VAN HORN CORRIDOR, DAVIS MOUNTAINS, AND MARFA PLATEAU... ...FIRE WEATHER WATCH IN EFFECT FROM LATE WEDNESDAY MORNING THROUGH EARLY WEDNESDAY EVENING FOR 20 FOOT WINDS OF 20 MPH OR GREATER, RELATIVE HUMIDITY BELOW 15 PERCENT, AND HIGH FIRE DANGER ACROSS GAINES COUNTY, THE SOUTHEAST NEW MEXICO PLAINS, UPPER TRANS PECOS, VAN HORN CORRIDOR, DAVIS MOUNTAINS, AND MARFA PLATEAU... ...FIRE WEATHER WATCH IN EFFECT FROM WEDNESDAY MORNING THROUGH WEDNESDAY EVENING FOR WIND AND LOW RELATIVE HUMIDITY FROM SOUTHEAST NEW MEXICO INTO GAINES COUNTY, TEXAS... * WINDS...Southwest 30 to 40 mph with gusts up to 60 mph Tuesday. Southwest winds 25 to 35 mph with gusts up to 50 mph Wednesday. * RELATIVE HUMIDITY...As low as 12 percent. * RFTI...5 or critical. * IMPACTS...Any fires that develop will likely spread rapidly. Outdoor burning is not recommended. * SEVERITY... FUELS (ERC)...25th-49th percentile...2 (out of 5). WEATHER...Near Critical...2 (out of 5). FIRE ENVIRONMENT...4 (out of 10).

INSTRUCTION: A Red Flag Warning means that critical fire weather conditions are either occurring now or will shortly. A combination of strong winds, low relative humidity and warm temperatures will increase potential for fire growth. A Fire Weather Watch means that critical fire weather conditions are forecast to occur. Listen for later forecasts and possible Red Flag Warnings.

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