Weather Alert in California

Recent Locations: Cylinder, IA   Lindsay, CA   Cranfills Gap, TX  
Current Alerts for Lindsay, CA: Extreme Heat Warning

Dust Advisory issued August 24 at 4:50PM PDT until August 24 at 5:15PM PDT by NWS Phoenix AZ

AREAS AFFECTED: Imperial, CA

DESCRIPTION: The National Weather Service in Phoenix has issued a * Dust Advisory for... South central Imperial County in southeastern California... * Until 515 PM PDT. * At 450 PM PDT, a wall of dust was along a line extending from near Brawley to near Mt. Signal, moving northeast at 35 mph. HAZARD...Less than one mile visibility with strong wind in excess of 50 mph. SOURCE...Doppler radar. IMPACT...Hazardous travel. * This includes the following highways... CA Interstate 8 between mile markers 42 and 60. CA Route 78 between mile markers 24 and 29. CA Route 111 between mile markers 9 and 19. Locations impacted include... Holtville and Bonds Corner.

INSTRUCTION: Blowing dust brings reduced visibility, leading to dangerous driving conditions. If driving, avoid blowing dust if possible. If caught in dense blowing dust, pull off the road, turn off your lights and keep your foot off the brake.

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Current U.S. National Radar--Current

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North America Water Vapor (Moisture)

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Weather Topic: What are Wall Clouds?

Home - Education - Cloud Types - Wall Clouds

Wall Clouds Next Topic: Altocumulus Clouds

A wall cloud forms underneath the base of a cumulonimbus cloud, and can be a hotbed for deadly tornadoes.

Wall clouds are formed by air flowing into the cumulonimbus clouds, which can result in the wall cloud descending from the base of the cumulonimbus cloud, or rising fractus clouds which join to the base of the storm cloud as the wall cloud takes shape.

Wall clouds can be very large, and in the Northern Hemisphere they generally form at the southern edge of cumulonimbus clouds.

Next Topic: Altocumulus Clouds

Weather Topic: What are Altostratus Clouds?

Home - Education - Cloud Types - Altostratus Clouds

Altostratus Clouds Next Topic: Cirrocumulus Clouds

Altostratus clouds form at mid to high-level altitudes (between 2 and 7 km) and are created by a warm, stable air mass which causes water vapor to condense as it rise through the atmosphere. Usually altostratus clouds are featureless sheets characterized by a uniform color.

In some cases, wind punching through the cloud formation may give it a waved appearance, called altostratus undulatus. Altostratus clouds are commonly seen with other cloud formations accompanying them.

Next Topic: Cirrocumulus Clouds

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