Weather Alert in New Mexico

Recent Locations: Sumter, SC   Aurora, ME   Embudo, NM  

Flood Watch issued August 30 at 12:53AM MDT until August 31 at 6:00AM MDT by NWS Albuquerque NM

AREAS AFFECTED: Curry County; Roosevelt County; De Baca County; Chaves County Plains; Eastern Lincoln County; Southwest Chaves County

DESCRIPTION: * WHAT...Flash flooding caused by excessive rainfall continues to be possible. * WHERE...Portions of central, east central, and southeast New Mexico, including the following areas, in central New Mexico, Eastern Lincoln County. In east central New Mexico, Curry County, De Baca County and Roosevelt County. In southeast New Mexico, Chaves County Plains and Southwest Chaves County. * WHEN...From noon MDT today through late tonight. * IMPACTS...Excessive runoff may result in flooding of rivers, creeks, streams, and other low-lying and flood-prone locations. Flooding may occur in poor drainage and urban areas. Extensive street flooding and flooding of creeks and rivers are possible. * ADDITIONAL DETAILS... - Above normal atmospheric moisture and impressive instability will combine to produce torrential rain producing storms Saturday afternoon and night. Rainfall rates in excess of 3 inches per hour are likely. This heavy rainfall will fall over already saturated grounds from Friday's heavy rainfall, increasing the flash flood threat. - http://www.weather.gov/safety/flood

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 Wall Clouds?

Home - Education - Cloud Types - Wall Clouds

Wall Clouds Next Topic: Altocumulus Clouds

A wall cloud forms underneath the base of a cumulonimbus cloud, and can be a hotbed for deadly tornadoes.

Wall clouds are formed by air flowing into the cumulonimbus clouds, which can result in the wall cloud descending from the base of the cumulonimbus cloud, or rising fractus clouds which join to the base of the storm cloud as the wall cloud takes shape.

Wall clouds can be very large, and in the Northern Hemisphere they generally form at the southern edge of cumulonimbus clouds.

Next Topic: Altocumulus Clouds

Weather Topic: What are Altostratus Clouds?

Home - Education - Cloud Types - Altostratus Clouds

Altostratus Clouds Next Topic: Cirrocumulus Clouds

Altostratus clouds form at mid to high-level altitudes (between 2 and 7 km) and are created by a warm, stable air mass which causes water vapor to condense as it rise through the atmosphere. Usually altostratus clouds are featureless sheets characterized by a uniform color.

In some cases, wind punching through the cloud formation may give it a waved appearance, called altostratus undulatus. Altostratus clouds are commonly seen with other cloud formations accompanying them.

Next Topic: Cirrocumulus Clouds

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