Weather Alert in Kansas
Red Flag Warning issued March 26 at 1:17PM CDT until March 27 at 8:00PM CDT by NWS Hastings NE
AREAS AFFECTED: Smith; Jewell; Osborne; Mitchell; Webster; Nuckolls; Thayer
DESCRIPTION: ...RED FLAG WARNING IN EFFECT FROM NOON TO 8 PM CDT FRIDAY... ...FIRE WEATHER WATCH IN EFFECT FROM SATURDAY MORNING THROUGH SATURDAY EVENING... The National Weather Service in Hastings has issued a Red Flag Warning for wind and low relative humidity, which is in effect from noon to 8 PM CDT Friday. A Fire Weather Watch has also been issued from Saturday morning through Saturday evening. * WINDS...Northeast 20 to 30 mph with gusts up to 40 mph this afternoon. North 15 to 20 mph with gusts to 30 MPH on Friday, and south 20 to 30 mph with gusts up to 45 mph on Saturday. * RELATIVE HUMIDITY...As low as 25 percent this afternoon. As low as 15 percent on Friday and Saturday afternoons. * IMPACTS...Any fire that develops will spread quickly. 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. 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 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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