Weather Alert in New Mexico
Fire Weather Watch issued February 15 at 12:14PM MST until February 17 at 7:00PM MST by NWS Albuquerque NM
AREAS AFFECTED: Northeast Plains; East Central Plains
DESCRIPTION: ...EXTENDED PERIOD OF RAPID FIRE SPREAD ACROSS EASTERN NEW MEXICO... .A storm system approaching from the west will allow south winds to increase on Monday. This combined with relative humidity values in the low teens will result in critical fire weather conditions across parts of northeast NM Monday 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. * AREA AND TIMING...Northeast Plains (Zone 104) and East-Central Plains (Zone 126) from late Tuesday morning through Tuesday afternoon. * 20 FOOT WINDS...Southwest to west 30 to 40 mph with peak gusts of 55 to 65 mph. * RELATIVE HUMIDITY...Minimum values of 14 to 25%. * 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 are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - 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
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