Weather Alert in California
Flash Flood Warning issued February 16 at 1:46PM PST until February 16 at 4:00PM PST by NWS Los Angeles/Oxnard CA
AREAS AFFECTED: Los Angeles, CA
DESCRIPTION: FFWLOX The National Weather Service in Los Angeles/Oxnard has extended the * Flash Flood Warning for... Southeastern Los Angeles County in southwestern California... * Until 400 PM PST. * At 146 PM PST, Doppler radar and automated rain gauges indicated thunderstorms producing heavy rain across the warned area. Between 1 and 2 inches of rain have fallen. Flash flooding is ongoing or expected to begin shortly. Rock slides and mud slides are expected. Minor debris flows possible on the Bridge Burn Scar. HAZARD...Flash flooding caused by thunderstorms. Rock slides and mud slides. Minor debris flows possible on the Bridge Burn Scar. SOURCE...Radar and automated gauges. IMPACT...Life threatening flash flooding. Thunderstorms producing flash flooding. Rock slides and mud slides. Minor debris flows possible on the Bridge Burn Scar. * Some locations that will experience flash flooding include... Long Beach, West Covina, Glendora, San Dimas, Pomona, Whittier, La Verne, Covina, Azusa, Baldwin Park, Diamond Bar, Hacienda Heights, Monrovia, Claremont, Santa Fe Springs, Norwalk, Cerritos, Artesia, Bellflower and Walnut.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Please report observed flooding to local emergency services or law enforcement and request they pass this information to the National Weather Service when you can do so safely.
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Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
Weather Topic: What are Cirrocumulus Clouds?
Home - Education - Cloud Types - Cirrocumulus Clouds
Next Topic: Cirrostratus Clouds
Cirrocumulus clouds form at high altitudes (usually around 5 km)
and have distinguishing characteristics displayed in a fine layer of
small cloud patches. These small cloud patches are sometimes referred to as
"cloudlets" in relation to the whole cloud formation.
Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the
water droplets in the cloud freeze into ice crystals and the cloud becomes a
cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud
formations generally pass rapidly.
Next Topic: Cirrostratus Clouds
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