Weather Alert in Colorado
Fire Weather Watch issued August 13 at 3:27AM MDT until August 14 at 10:00PM MDT by NWS Pueblo CO
AREAS AFFECTED: Upper Arkansas River Valley Including Lake County and Chaffee County; Fremont County Including Canon City/Howard/Texas Creek; Eastern San Juan Mountains and La Garita Mountains Including Wolf Creek Pass and Creede; Southern Front Range Including Sangre De Cristo Mountains/Wet Mountains/La Veta Pass
DESCRIPTION: ...Fire Weather Watch has been issued across the central, southwest and southeast mountains from Thursday afternoon through Thursday evening for dry thunderstorms... * AFFECTED AREA...Fire Weather Zones 220, 222, 223 and 225. * IMPACTS...Any fire that develops will catch and spread quickly. Outdoor burning is not recommended. * Thunderstorms...Scattered high based thunderstorms will be possible Thursday afternoon and evening. Storms will be capable of producing lightning and gusty outflow winds, with little measurable rainfall.
INSTRUCTION: A Fire Weather Watch means that critical fire weather conditions are forecast to occur. Listen for later forecasts and possible Red Flag Warnings.
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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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