Weather Alert in Oregon
Winter Weather Advisory issued March 31 at 10:42AM PDT until April 2 at 11:00AM PDT by NWS Medford OR
AREAS AFFECTED: Klamath Basin; Northern and Eastern Klamath County and Western Lake County
DESCRIPTION: * WHAT...Snow and gusty winds expected. Total snow accumulations 3 to 6 inches. Winds gusts up to 25 mph at lower elevations with gusts up to 45 mph over higher terrain are expected. * WHERE...Northern Klamath Basin, northern and eastern Klamath County and far western Lake County. This includes Highway 97 from Modoc Point northward and the higher portions of Highway 140 between Bly and Lakeview. This includes the communities of Chiloquin, Chemult, and Crescent and the higher terrain in eastern Klamath and western Lake counties. * WHEN...From 5 PM Wednesday to 11 AM PDT Thursday. * IMPACTS...Travel may be difficult and delays in your commute. The hazardous conditions could impact the Wednesday evening and Thursday morning commutes. Gusty winds could bring down tree branches.
INSTRUCTION: Slow down and use caution while traveling. Call 511 or visit tripcheck.com for road information.
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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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