Weather Alert in Oregon

Recent Locations: Running Springs, CA   Kerrville, TX   Saint Paul, OR  

Winter Storm Watch issued February 15 at 4:39AM PST until February 17 at 10:00PM PST by NWS Medford OR

AREAS AFFECTED: Eastern Curry County and Josephine County

DESCRIPTION: * WHAT...Heavy snow possible above 2000 ft. Total snow accumulations 8 to 12 inches possible. * WHERE...Eastern Curry County and portions of Josephine County above 2000 ft. This includes the Kalmiopsis Region and Bear Camp Rd. * WHEN...From Monday evening through Tuesday evening. * IMPACTS...Travel may be very difficult to impossible. The hazardous conditions could impact the Tuesday morning and evening commutes. * ADDITIONAL DETAILS...The heaviest snow is expected Monday night into early Tuesday morning.

INSTRUCTION: Monitor the latest forecasts for updates on this situation.

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Weather Topic: What are Stratocumulus Clouds?

Home - Education - Cloud Types - Stratocumulus Clouds

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

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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