Weather Alert in Nevada
Wind Advisory issued March 14 at 2:03AM PDT until March 14 at 8:00PM PDT by NWS Reno NV
AREAS AFFECTED: Mineral and Southern Lyon Counties
DESCRIPTION: * WHAT...West winds 20 to 30 mph with gusts 45 to 50 mph, and gusts up to 50 to 60 mph along Highway 95 from Hawthorne to Schurz. * WHERE...Mineral and Southern Lyon Counties. * WHEN...From 11 AM this morning to 8 PM PDT this evening. * IMPACTS...Difficult driving conditions are expected, especially for high-profile vehicles along US-95. Gusty winds will blow around unsecured objects. Tree limbs could be blown down and a few power outages may result. * ADDITIONAL DETAILS...The strongest winds will be between 1 PM and 5 PM in the vicinity of Walker Lake.
INSTRUCTION: Now is the time to secure loose outdoor items such as patio furniture, holiday decorations, and trash cans before winds increase which could blow these items away.
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North America Water Vapor (Moisture)
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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
