Weather Alert in Missouri

Recent Locations: Empire, CA   Manchester, VT   Fredericktown, MO  

Hydrologic Outlook issued May 8 at 3:27AM CDT by NWS Kansas City/Pleasant Hill MO

AREAS AFFECTED: Cass, MO; Henry, MO; Johnson, MO

DESCRIPTION: ESFEAX Big Creek at Blairstown 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: Big Creek at Blairstown Flood stage: 20.0 feet Latest stage: 15.3 feet at 3 AM Thursday Maximum Forecast Stage: 22.1 feet at 8 PM Thursday May 08 Fld Obs Forecasts Location Stg Stg Day/Time Thu Thu Fri 4am 4pm 4am Big Creek Blairstown 20.0 15.3 Thu 3am 17.1 22.0 22.0 Later statements, possibly warnings, may be issued as additional information becomes available.

INSTRUCTION: N/A

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Weather Topic: What is Sleet?

Home - Education - Precipitation - Sleet

Sleet Next Topic: Snow

Sleet is a form of precipitation in which small ice pellets are the primary components. These ice pellets are smaller and more translucent than hailstones, and harder than graupel. Sleet is caused by specific atmospheric conditions and therefore typically doesn't last for extended periods of time.

The condition which leads to sleet formation requires a warmer body of air to be wedged in between two sub-freezing bodies of air. When snow falls through a warmer layer of air it melts, and as it falls through the next sub-freezing body of air it freezes again, forming ice pellets known as sleet. In some cases, water droplets don't have time to freeze before reaching the surface and the result is freezing rain.

Next Topic: Snow

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

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