Weather Alert in Florida
Red Flag Warning issued February 22 at 1:15AM EST until February 22 at 7:00PM EST by NWS Tallahassee FL
AREAS AFFECTED: Inland Franklin; Leon; Inland Jefferson; Madison; Inland Wakulla; Inland Taylor; Lafayette; Inland Dixie; Coastal Franklin; Coastal Jefferson; Coastal Wakulla; Coastal Taylor; Coastal Dixie; Southern Liberty
DESCRIPTION: ...RED FLAG WARNING IN EFFECT FOR THE FL BIG BEND THIS AFTERNOON AND EVENING DUE TO CRITICALLY LOW HUMIDITY AND GUSTY WINDS... .A very dry airmass and gusty northwest winds are on tap this afternoon and evening. Critically low relative humidity, along with strong winds and dry fuels from the ongoing drought, are expected to result in red flag conditions this afternoon and evening. * AFFECTED AREA...Fire weather zones 015, 017, 018, 019, 027, 028, 029, 034, 115, 118, 127, 128, 134, and 426. * WIND...Northwest winds 16 to 22 mph with gusts of 25 to 30 mph. * HUMIDITY...As low as 25 percent. * IMPACTS...Any fires that develop will likely spread rapidly. Outdoor burning is not recommended.
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 can contribute to extreme fire behavior.
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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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