Weather Alert in Kansas

Recent Locations: Springfield, SD   Mapleton, IL   Alta Vista, KS  

Hydrologic Outlook issued August 27 at 8:01AM CDT by NWS Topeka KS

AREAS AFFECTED: Lyon, KS

DESCRIPTION: ESFTOP Cottonwood River near Emporia This hydrologic outlook is based on the forecast rainfall for the next 24 hours and estimated runoff from earlier rainfall. Crests may vary if actual rainfall or runoff is greater or less than anticipated. Location: Cottonwood River near Emporia Flood stage: 20.0 feet Latest stage: 2.6 feet at 7 AM Wednesday Maximum Forecast Stage: 22.7 feet at 7 PM Friday Aug 29 Fld Obs Forecasts Location Stg Stg Day/Time Wed Thu Fri 1pm 1pm 1pm Cottonwood River Emporia 20.0 2.6 Wed 7am 2.6 13.5 22.5 Later statements, possibly warnings, may be issued as additional information becomes available.

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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