Weather Alert in California

Special Weather Statement issued July 29 at 9:13PM PDT by NWS San Diego CA

AREAS AFFECTED: San Diego County Coastal Areas; Orange County Coastal

DESCRIPTION: ...TSUNAMI ADVISORY IS IN EFFECT FOR COASTAL AREAS OF ORANGE AND SAN DIEGO COUNTIES... * LOCAL IMPACTS... For people in the advisory area...A tsunami capable of producing strong currents that may be hazardous to swimmers, boats, and coastal structures is expected. Widespread inundation is NOT expected. * RECOMMENDED ACTIONS... For people in the advisory area...If you are located in this coastal area, move off the beach and out of harbors and marinas. Do not go to the coast to watch the tsunami. Be alert to instructions from your local emergency officials * FORECAST TSUNAMI START TIMES... Newport Beach California 0110 AM PDT on Jul 30 La Jolla California 0110 AM PDT on Jul 30 Oceanside California 0115 AM PDT on Jul 30 Tsunamis often arrive as a series of waves or surges which could be dangerous for many hours after the first wave arrival. The first tsunami wave or surge may not be the highest in the series. * FORECAST PEAK TSUNAMI WAVE HEIGHTS... Newport Beach California less than 1 ft La Jolla California less than 1 ft Oceanside California less than 1 ft * PRELIMINARY EARTHQUAKE INFORMATION... An earthquake occurred with a preliminary magnitude of 8.8. * TIDE INFORMATION... Newport Beach...High 4.0 feet (MLLW) 01:59 AM PDT. Low 1.2 feet (MLLW) 08:15 AM PDT. La Jolla...High 4.0 feet (MLLW) 01:51 AM PDT. Low 1.3 feet (MLLW) 08:09 AM PDT. This product will be updated as new information becomes available. Stay tuned to your local news source and NOAA weather radio for further information and updates.

INSTRUCTION: N/A

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Weather Topic: What are Contrails?

Home - Education - Cloud Types - Contrails

Contrails Next Topic: Cumulonimbus Clouds

A contrail is an artificial cloud, created by the passing of an aircraft.

Contrails form because water vapor in the exhaust of aircraft engines is suspended in the air under certain temperatures and humidity conditions. These contrails are called exhaust contrails.

Another type of contrail can form due to a temporary reduction in air pressure moving over the plane's surface, causing condensation. These are called aerodynamic contrails.

When you can see your breath on a cold day, it is also because of condensation. The reason contrails last longer than the condensation from your breath is because the water in contrails freezes into ice particles.

Next Topic: Cumulonimbus Clouds

Weather Topic: What are Cumulus Clouds?

Home - Education - Cloud Types - Cumulus Clouds

Cumulus Clouds Next Topic: Drizzle

Cumulus clouds are fluffy and textured with rounded tops, and may have flat bottoms. The border of a cumulus cloud is clearly defined, and can have the appearance of cotton or cauliflower.

Cumulus clouds form at low altitudes (rarely above 2 km) but can grow very tall, becoming cumulus congestus and possibly the even taller cumulonimbus clouds. When cumulus clouds become taller, they have a greater chance of producing precipitation.

Next Topic: Drizzle

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