Weather Alert in Washington

Recent Locations: Fall City, WA   Crockett, CA   Mansfield, OH  
Current Alerts for Fall City, WA: Winter Storm Warning

Flood Warning issued March 12 at 11:19AM PDT until March 14 at 8:00PM PDT by NWS Spokane WA

AREAS AFFECTED: Chelan, WA

DESCRIPTION: * WHAT...Flooding caused by rain and snowmelt is expected for the lower Stehekin Valley. * WHERE...A portion of North Central Washington, including Chelan county. * WHEN...Until 800 PM PDT Saturday. * IMPACTS...When the Stehekin River gauge hits 19.3 feet, water breaches the river bank. At 20 feet, water inundates some properties and overtops the temporary corduroy bridge. Company Creek Road is beginning to flood in places at the northern end. Battalion Creek culverts are beginning to be overtopped. At 20.5 feet, water begins to damage Wood Road. * ADDITIONAL DETAILS... - At 1114 AM PDT, the Stehekin River was above Action Stage (19.5 feet). Flooding is ongoing or expected the warned area. - Additional rainfall amounts of 0.5 to 1.5 inches are possible in the warned area through Saturday evening. A period of moderate to heavy rain and high winds will lead to snowmelt. Another peak of 19.8 feet is forecast Friday morning before receeding below Action stage Sunday. - Some locations that will experience flooding include... Company Creek Campground. - http://www.weather.gov/safety/flood

INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles.

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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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