Weather Alert in New Mexico

Recent Locations: Zirconia, NC   Desha, AR   Nogal, NM  
Current Alerts for Nogal, NM: Wind Advisory

Red Flag Warning issued February 20 at 2:36AM MST until February 20 at 6:00PM MST by NWS Albuquerque NM

AREAS AFFECTED: Northeast Plains; Central Highlands; East Central Plains

DESCRIPTION: ...RED FLAG WARNING TODAY FROM 9 AM TO 6 PM FOR THE NORTHEAST AND EAST CENTRAL PLAINS, AND CENTRAL HIGHLANDS, DUE TO STRONG WINDS AND LOW HUMIDITY... .Persistently strong flow aloft, an area of low pressure at the surface over the northeast corner of New Mexico, and very dry fuels over northeast and east central parts of the state will result in critical fire weather conditions again today. Wind speeds will be stronger today than they were Thursday, with westerly gusts reaching 50 to 60 mph. * AREA AND TIMING...Northeast Plains (Zone 104), East Central Plains (Zone 126), and Central Highlands (Zone 125) today from 9 AM to 6 PM MST. * 20 FOOT WINDS...West winds 25 to 40 mph with gusts up to 60 mph. * RELATIVE HUMIDITY...Minimum values between 12 and 19 percent. * 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.

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Weather Topic: What are Wall Clouds?

Home - Education - Cloud Types - Wall Clouds

Wall Clouds Next Topic: Altocumulus Clouds

A wall cloud forms underneath the base of a cumulonimbus cloud, and can be a hotbed for deadly tornadoes.

Wall clouds are formed by air flowing into the cumulonimbus clouds, which can result in the wall cloud descending from the base of the cumulonimbus cloud, or rising fractus clouds which join to the base of the storm cloud as the wall cloud takes shape.

Wall clouds can be very large, and in the Northern Hemisphere they generally form at the southern edge of cumulonimbus clouds.

Next Topic: Altocumulus Clouds

Weather Topic: What are Altostratus Clouds?

Home - Education - Cloud Types - Altostratus Clouds

Altostratus Clouds Next Topic: Cirrocumulus Clouds

Altostratus clouds form at mid to high-level altitudes (between 2 and 7 km) and are created by a warm, stable air mass which causes water vapor to condense as it rise through the atmosphere. Usually altostratus clouds are featureless sheets characterized by a uniform color.

In some cases, wind punching through the cloud formation may give it a waved appearance, called altostratus undulatus. Altostratus clouds are commonly seen with other cloud formations accompanying them.

Next Topic: Cirrocumulus Clouds

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