Weather Alert in Oregon

Recent Locations: Point Arena, CA   Clarks, NE   Independence, OR  

Freeze Watch issued February 18 at 2:52PM PST until February 20 at 9:00AM PST by NWS Medford OR

AREAS AFFECTED: South Central Oregon Coast; Curry County Coast

DESCRIPTION: * WHAT...Sub-freezing temperatures as low as 24 degrees are possible, but lows of 28 to 32 degrees are more likely along the immediate coast and beaches. * WHERE...The coast of Douglas, Coos, and Curry counties. This includes Reedsport, Lakeside, Charleston, Coquille, Bandon, Port Orford, Gold Beach, and Brookings. * WHEN...From late Thursday night through Friday morning. * IMPACTS...Frost and freezing conditions could kill crops, other sensitive vegetation and possibly damage unprotected outdoor plumbing.

INSTRUCTION: Take steps now to protect tender plants from the cold. To prevent water pipes from freezing; wrap or drain or allow them to drip slowly.

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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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