Weather Alert in New Mexico
Flood Watch issued August 24 at 10:04PM MDT until August 26 at 6:00AM MDT by NWS Albuquerque NM
AREAS AFFECTED: Southern Sangre de Cristo Mountains; East Slopes Sangre de Cristo Mountains; Far Northeast Highlands; Northeast Highlands; Harding County; Eastern San Miguel County
DESCRIPTION: * WHAT...Flash flooding caused by excessive rainfall continues to be possible. * WHERE...Portions of north central and northeast New Mexico, including the following areas, in north central New Mexico, East Slopes Sangre de Cristo Mountains and Southern Sangre de Cristo Mountains. In northeast New Mexico, Eastern San Miguel County, Far Northeast Highlands, Harding County and Northeast Highlands. This includes the Hermits Peak-Calf Canyon wildfire burn scar area. * WHEN...From Monday afternoon through late Monday night. * 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. Low-water crossings may be flooded. * ADDITIONAL DETAILS... - Atmospheric moisture will increase even more into Monday as a weak frontal boundary moves in from the northeast. Numerous storms capable of very heavy rainfall rates will develop, increasing the risk of excessive runoff and flash flooding. The Hermits Peak-Calf Canyon wildfire burn scar area will be especially vulnerable to 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 is Condensation?
Home - Education - Precipitation - Condensation
Next Topic: Contrails
Condensation is the process which creates clouds, and therefore
it is a crucial process in the water cycle.
Condensation is the change of matter from a state of gas into a state of liquid,
and it happens because water molecules release heat into the atmosphere and
become organized into a more closely packed structure, what we might see as
water droplets.
Water is always present in the air around us as a vapor, but it's too small for
us to see. When water undergoes the process of condensation it becomes organized
into visible water droplets. You've probably seen condensation happen before on the
surface of a cold drink!
Next Topic: Contrails
Weather Topic: What are Cumulonimbus Clouds?
Home - Education - Cloud Types - Cumulonimbus Clouds
Next Topic: Cumulus Clouds
The final form taken by a growing cumulus cloud is the
cumulonimbus cloud, which is very tall and dense.
The tower of a cumulonimbus cloud can soar 23 km into the atmosphere, although
most commonly they stop growing at an altitude of 6 km.
Even small cumulonimbus clouds appear very large in comparison to other cloud types.
They can signal the approach of stormy weather, such as thunderstorms or blizzards.
Next Topic: Cumulus Clouds
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