Weather Alert in Missouri
Hydrologic Outlook issued June 24 at 9:18AM CDT by NWS Kansas City/Pleasant Hill MO
AREAS AFFECTED: Daviess, MO; Livingston, MO
DESCRIPTION: ESFEAX Grand River near Gallatin 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: Grand River near Gallatin Flood stage: 26.0 feet Latest stage: 3.8 feet at 8 AM Tuesday Maximum Forecast Stage: 27.5 feet at 7 AM Thursday Jun 26 Fld Obs Forecasts Location Stg Stg Day/Time Tue Wed Thu 1pm 1pm 1pm Grand River Gallatin 26.0 3.8 Tue 8am 3.8 15.7 27.5 Later statements, possibly warnings, may be issued as additional information becomes available.
INSTRUCTION: N/A
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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