Weather Alert in California
Heat Advisory issued June 7 at 1:23PM PDT until June 9 at 11:00PM PDT by NWS Sacramento CA
AREAS AFFECTED: Shasta Lake Area / Northern Shasta County; Northern Sacramento Valley; Northeast Foothills/Sacramento Valley
DESCRIPTION: * WHAT...Hot temperatures 102 to 108 and areas of Major HeatRisk expected. Limited overnight relief with low temperatures in the low to mid 70s. * WHERE...Northeast Foothills, Northern Sacramento Valley, and Shasta Lake Area / Northern Shasta County. * WHEN...From 11 AM Sunday to 11 PM PDT Monday. * IMPACTS...Heat related illnesses increase significantly during extreme heat events, particularly for those working or participating in outdoor activities. * ADDITIONAL DETAILS...Area waterways continue to run cold and fast, creating dangerous conditions for those seeking relief in rivers and lakes.
INSTRUCTION: Drink plenty of fluids, stay in an air-conditioned room, stay out of the sun, and check up on relative and neighbors, especially those more susceptible to heat impacts.
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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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