Weather Alert in Nevada
Hydrologic Outlook issued August 23 at 1:45PM PDT by NWS Elko NV
AREAS AFFECTED: Elko, NV; Eureka, NV
DESCRIPTION: ESFLKN Deep monsoonal moisture will surge north into northern and central Nevada Sunday afternoon through Wednesday evening. This will support daily rounds of showers and thunderstorms each afternoon and evening. Slow storm motions may produce heavy rainfall and localized flooding. Of particular concern are recent large burn scars, including the Snowstorm Complex near Midas, the Cottonwood Peak Fire north of Tuscarora, the Hot Canyon Fire northwest of Montello, and the Adobe Fire north of Elko. Numerous smaller burn scars from this fire season also remain vulnerable. Residents near recent burned scars should have multiple ways to receive flash flood warnings and be prepared to act quickly. Travelers and recreationists in these areas should also remain alert and consider alternate plans.
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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