Weather Alert in New Mexico
Flood Advisory issued July 3 at 1:38AM MDT until July 3 at 4:30AM MDT by NWS El Paso Tx/Santa Teresa NM
AREAS AFFECTED: Grant, NM; Luna, NM
DESCRIPTION: * WHAT...Areal flooding caused by earlier excessive rainfall is expected to continue into the early morning hours. * WHERE...Portions of Luna County in New Mexico. * WHEN...Until 430 AM MDT. * IMPACTS...Water over roadways, large areas of ponding, and flooding of poor drainage areas. * ADDITIONAL DETAILS... - At 138 AM MDT, Department of Transportation officials reported flooding in places along U.S. Highway 180 northwest of Deming, and south of the Highway 35 junction. Earlier heavy rainfall west of Cookes Peak fell in an area of poorly defined drainage, and runoff flooding may try to extend south towards the low-lying residential areas north of Deming, between Highway 26 and the Hidden Valley Road. - Flooding impacts will continue, but no additional rainfall is expected. - Some locations that may experience flooding include... Areas between Deming and Butterfield Trail Estates, including portions of U.S. Highway 180. - http://www.weather.gov/safety/flood
INSTRUCTION: Be especially cautious at night when it is harder to recognize the dangers of flooding. Be aware of your surroundings and do not drive on flooded roads.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
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Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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