Weather Alert in Oregon
Flood Watch issued February 23 at 10:01AM PST until February 25 at 4:00AM PST by NWS Medford OR
AREAS AFFECTED: South Central Oregon Coast
DESCRIPTION: ...The National Weather Service in Medford OR has issued a Flood Watch for the following rivers in Oregon... South Fork Coquille River at Myrtle Point affecting South Central Oregon Coast zone. .A Pineapple Express will bring heavy rain to the Coquille River basin, which could result in minor flooding due to excessive runoff. * WHAT...Minor flooding is possible. * WHERE...South Fork Coquille River at Myrtle Point. * WHEN...Through early Wednesday morning. The river is expected to crest Tuesday afternoon. * IMPACTS...At 30.0 feet, Agricultural and pasture land begins to flood. Impacts on cattle grazing are possible. * ADDITIONAL DETAILS... - At 9:20 AM PST Monday the stage was 24.0 feet. - Forecast...Flood stage may be reached based on the latest forecast information. - Flood stage is 33.0 feet. - http://www.weather.gov/safety/flood
INSTRUCTION: If you are in the watch area, remain alert to possible flooding. Additional information is available at www.weather.gov. The next statement will be issued Tuesday morning at 1000 AM PST.
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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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