Weather Alert in New Mexico
Flood Watch issued August 26 at 11:10AM MDT until August 27 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 continues to be possible. * 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. * WHEN...Through this evening. * 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... - Numerous thunderstorms will develop over the northern mountains this afternoon and evening, with scattered to numerous coverage of storms over the south central mountains. Some of the stronger storms will be capable of producing rain at rates over 1 inch per hour, and some locations may receive multiple storms. Locations where the ground is already saturated from heavy rainfall, recent burn scars, and urban areas will be especially susceptible to rapid runoff and flash flooding. On Monday, the western third of the San Miguel County part of the Hermits Peak Calf Canyon scar accumulated 1 to 2 inches of rainfall, so rapid runoff is likely there today. - 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
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
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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