Weather Alert in Oklahoma

Recent Locations: Glenpool, OK  
Current Alerts for Glenpool, OK: Flood Advisory

Flood Warning issued June 17 at 2:58AM CDT until June 20 at 11:40PM CDT by NWS Tulsa OK

AREAS AFFECTED: Okmulgee, OK

DESCRIPTION: ...The Flood Warning continues for the following rivers in Oklahoma... Deep Fork River near Beggs affecting Okmulgee County. * WHAT...Minor flooding is forecast. * WHERE...Deep Fork River near Beggs. * WHEN...From late Wednesday night to late Friday evening. * IMPACTS...At 20.0 feet, minor flooding of agricultural lands occurs. Webster Road north of the gage site becomes impassable as well as some other county roads south of Beggs. * ADDITIONAL DETAILS... - At 2:15 AM CDT Tuesday the stage was 12.2 feet. - Forecast...The river is expected to rise above flood stage early Thursday morning to a crest of 19.6 feet Thursday evening. It will then fall below flood stage Friday afternoon. - Flood stage is 18.0 feet. - http://www.weather.gov/safety/flood

INSTRUCTION: N/A

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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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