Weather Alert in New Mexico
Fire Weather Watch issued March 24 at 12:11PM MDT until March 26 at 8:00PM MDT by NWS Albuquerque NM
AREAS AFFECTED: Northeast Plains; Sangre de Cristo Mountains; Northeast Highlands; Central Highlands
DESCRIPTION: ...FIRE WEATHER WATCH THURSDAY FROM 11 AM UNTIL 8 PM MDT FOR AREAS ALONG AND EAST OF THE CENTRAL MOUNTAIN CHAIN DUE TO RECORD HEAT, STRONG WINDS, AND LOW HUMIDITY... .Amidst an extended stretch of record high temperatures, west winds will strengthen Thursday in response to an upper level trough passing eastward along the Colorado and New Mexico border, and a potent surface trough in the lee of the Sangre de Cristo Mountains. Winds will gust up to 45 mph as humidity values plummet into the single-digits and high temperatures reach around 25 to 30 degrees above average. * AREA AND TIMING...Northeast Plains (Zone 104), Sangre de Cristo Mountains (Zone 122), Northeast Highlands (Zone 123), and Central Highlands (Zone 125) Thursday from 11 AM until 8 PM MDT. * 20 FOOT WINDS...West and southwest winds 25 to 30 mph with gusts up to 45 mph. * RELATIVE HUMIDITY...Minimum values around 4 to 6 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 Fire Weather Watch.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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