Weather Alert in Alaska
Special Weather Statement issued February 4 at 10:48AM AKST by NWS Fairbanks AK
AREAS AFFECTED: Western Arctic Coast; Northwest Arctic Coast; Northern Arctic Coast; Central Beaufort Sea Coast; Eastern Beaufort Sea Coast; Western Arctic Plains; Central Arctic Plains
DESCRIPTION: Wind gusts around 30 to 40 mph will continue across the Arctic Coast through tonight (locally higher around Point Hope up to 60 mph), leading to areas of blowing snow and very cold wind chills. Winds will gradually lessen on Thursday for Central/Eastern regions as strongest winds shift to being confined to the Western Arctic Coast. Given air temperatures in the -10F to -40F range, wind chills will be even colder down to around -40F to -55F.
INSTRUCTION: N/A
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North America Water Vapor (Moisture)
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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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