Weather Alert in Arizona
Winter Storm Warning issued February 19 at 2:00PM MST until February 20 at 5:00AM MST by NWS Flagstaff AZ
AREAS AFFECTED: Kaibab Plateau
DESCRIPTION: * WHAT...Snow showers will develop later today, becoming heavy at times through the evening, before tapering off a few hours after Midnight MST. Most areas will see general accumulations 4 to 8 inches, locally more south of Jacob Lake. Southwest through west winds gusting as high as 40 mph will create areas of blowing and drifting snow. * WHERE...Kaibab Plateau. * WHEN...From 5 PM this afternoon to 5 AM MST Friday. * IMPACTS...Roads, and especially bridges, will likely become slick and hazardous. Travel is not recommended as heavy snowfall and low visibility will create dangerous driving conditions. * ADDITIONAL DETAILS... Forecast snowfall amounts from 5 PM MST Today to 5 AM MST Friday... Fredonia: 2 to 4" Jacob Lake: 6 to 8"
INSTRUCTION: If you must travel, keep an extra flashlight, food, and water in your vehicle in case of an emergency. For the latest road conditions and closures go to az511.gov, or call 5 1 1. Persons should consider delaying all travel. Motorists should use extreme caution if travel is absolutely necessary.
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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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