Weather Alert in Montana
Winter Storm Warning issued March 11 at 2:15PM MDT until March 15 at 6:00AM MDT by NWS Billings MT
AREAS AFFECTED: Absaroka/Beartooth Mountains
DESCRIPTION: * WHAT...Prolonged periods of heavy snow possible. Total snow accumulations between 1 and 3 feet possible, greatest on south and west facing aspects. Winds could gust as high as 85 mph Thursday. * WHERE...Absaroka/Beartooth Mountains. * WHEN...From 6 PM this evening to 6 AM MDT Sunday. * IMPACTS...Recreation in the high country could be severely impacted by heavy accumulating snow. Travel could be very difficult to impossible. Widespread blowing snow could significantly reduce visibility. Very strong winds could cause extensive damage to trees and power lines. * ADDITIONAL DETAILS...Snow will begin this evening on south and west facing aspects. Snow may not begin falling on the north aspects until Thursday night or Friday.
INSTRUCTION: Do not get caught unprepared in the high country. Severe winter conditions are expected. Avalanche danger will also increase.
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Weather Topic: What is Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - Shelf Clouds
Next Topic: Sleet
A shelf cloud is similar to a wall cloud, but forms at the front
of a storm cloud, instead of at the rear, where wall clouds form.
A shelf cloud is caused by a series of events set into motion by the advancing
storm; first, cool air settles along the ground where precipitation has just fallen.
As the cool air is brought in, the warmer air is displaced, and rises above it,
because it is less dense. When the warmer air reaches the bottom of the storm cloud,
it begins to cool again, and the resulting condensation is a visible shelf cloud.
Next Topic: Sleet
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