Weather Alert in New Mexico
Flood Watch issued June 30 at 6:40PM MDT until July 1 at 12:00AM MDT by NWS Albuquerque NM
AREAS AFFECTED: Southern Sangre de Cristo Mountains; East Slopes Sangre de Cristo Mountains; South Central Mountains; Northeast Highlands
DESCRIPTION: * WHAT...Flash flooding caused by excessive rainfall. * WHERE...Portions of central, north central, and northeast New Mexico, including the following areas, in central New Mexico, South Central Mountains. In north central New Mexico, East Slopes Sangre de Cristo Mountains and Southern Sangre de Cristo Mountains. In northeast New Mexico, Northeast Highlands. This includes Ruidoso and the burn scars surrounding the village as well as areas within and downstream of the Hermits Peak Calf Canyon burn scar. * WHEN...Until midnight MDT tonight. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Creeks and streams may rise out of their banks. Storm drains and ditches may become clogged with debris. * ADDITIONAL DETAILS... - Slow moving thunderstorms with rainfall rates of 1 to 2 inches per hour will create a high risk for burn scar flash flooding. - http://www.weather.gov/abq/EmergencyPrepFlood
INSTRUCTION: You should monitor later forecasts and be prepared to take action should Flash Flood Warnings be issued.
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Weather Topic: What are Cirrus Clouds?
Home - Education - Cloud Types - Cirrus Clouds
Next Topic: Condensation
Cirrus clouds are high-level clouds that occur above 20,000 feet
and are composed mainly of ice crystals.
They are thin and wispy in appearance.
What do they indicate?
They are often the first sign of an approaching storm.
Next Topic: Condensation
Weather Topic: What are Contrails?
Home - Education - Cloud Types - 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
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