Weather Alert in Texas
Fire Weather Watch issued March 28 at 12:40AM CDT until March 29 at 7:00PM CDT by NWS Lake Charles LA
AREAS AFFECTED: Tyler; Hardin; Northern Jasper; Northern Newton; Southern Jasper; Southern Newton; Upper Jefferson; Northern Orange; Lower Jefferson; Southern Orange
DESCRIPTION: ...RED FLAG WARNING FOR SOUTHWEST LOUISIANA... .Windy and dry conditions behind a cold front may produce red flag conditons across much of the area Monday. * AFFECTED AREA...Fire Weather Zone 180 Tyler, Fire Weather Zone 201 Hardin, Fire Weather Zone 259 Northern Jasper, Fire Weather Zone 260 Northern Newton, Fire Weather Zone 261 Southern Jasper, Fire Weather Zone 262 Southern Newton, Fire Weather Zone 515 Upper Jefferson, Fire Weather Zone 516 Northern Orange, Fire Weather Zone 615 Lower Jefferson and Fire Weather Zone 616 Southern Orange. * TIMING...From Sunday morning through Sunday evening. * WINDS...South 5 to 10 mph. * RELATIVE HUMIDITY...As low as 35 percent. * TEMPERATURES...Up to 82. * IMPACTS...Any fire that develops will catch and spread quickly. Outdoor burning is not recommended.
INSTRUCTION: A Fire Weather Watch means that critical fire weather conditions are forecast to occur. Listen for later forecasts and possible Red Flag Warnings.
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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
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - 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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