Weather Alert in California

Recent Locations: Covelo, CA  
Current Alerts for Covelo, CA: Frost Advisory Wind Advisory

Frost Advisory issued May 8 at 3:13AM PDT until May 8 at 9:00AM PDT by NWS Eureka CA

AREAS AFFECTED: Southern Trinity; Northeastern Mendocino Interior

DESCRIPTION: * WHAT...For the Frost Advisory, temperatures as low as 33 will result in frost formation. For the Wind Advisory, northeast winds 25 to 35 mph with gusts up to 55 mph expected. * WHERE...Northeastern Mendocino Interior and Southern Trinity. * WHEN...For the Frost Advisory, until 9 AM PDT this morning. For the Wind Advisory, from 8 PM this evening to 9 AM PDT Thursday. * IMPACTS...Frost could harm sensitive outdoor vegetation. Sensitive outdoor plants may be killed if left uncovered. Wind gusts will be particularly strong along windward ridges and exposed coastal headlands.

INSTRUCTION: Winds this strong can make driving difficult, especially for high profile vehicles. Use extra caution. Take steps now to protect tender plants from the cold.

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Weather Topic: What is Precipitation?

Home - Education - Precipitation - 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.

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Weather Topic: What are Shelf Clouds?

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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.

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