Weather Alert in California
Flash Flood Warning issued February 16 at 3:20PM PST until February 16 at 5:00PM 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... Southwestern Los Angeles County in southwestern California... * Until 500 PM PST. * At 320 PM PST, Doppler radar and automated rain gauges indicate that another round of moderate to heavy rainfall will move over the warned area soon. Flash flooding is ongoing or expected to begin shortly. HAZARD...Flash flooding caused by thunderstorms. SOURCE...Radar and automated gauges. IMPACT...Flash flooding of small creeks and streams, urban areas, highways, streets and underpasses as well as other poor drainage and low-lying areas. Rock and mud slides. Minor debris flows at recent burn scars including the Eaton burn scar. * Some locations that will experience flash flooding include... Long Beach, Downtown Los Angeles, Griffith Park, Hollywood, Inglewood, Culver City, Burbank, Alhambra, North Hollywood, Pasadena, Venice, Santa Monica, Manhattan Beach, Van Nuys, Hermosa Beach, Torrance, Encino, Redondo Beach, Mount Wilson, and Eaton Burn Scar.
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles. Be aware of your surroundings and do not drive on flooded roads, and be aware of rock slides and mud slides around high terrain. Follow direction of Emergency Management and Law Enforcement officials.
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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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