Weather Alert in New Mexico

Recent Locations: Belfield, ND   Boswell, PA   Santa Rosa, NM  
Current Alerts for Santa Rosa, NM: High Wind Warning

Wind Advisory issued February 17 at 8:46PM MST until February 18 at 8:00PM MST by NWS El Paso Tx/Santa Teresa NM

AREAS AFFECTED: Upper Gila River Valley; Southern Gila Foothills/Mimbres Valley; Southwest Desert/Lower Gila River Valley; Lowlands of the Bootheel; Uplands of the Bootheel; Southwest Desert/Mimbres Basin; Eastern Black Range Foothills; Sierra County Lakes; Northern Dona Ana County; Southern Dona Ana County/Mesilla Valley; West Slopes Sacramento Mountains Below 7500 Feet; Otero Mesa; Central Grant County/Silver City Area; East Central Tularosa Basin/Alamogordo; Southeast Tularosa Basin; Western El Paso County; Northern Hudspeth Highlands/Hueco Mountains; Salt Basin; Rio Grande Valley of Eastern El Paso/Western Hudspeth Counties

DESCRIPTION: * WHAT...Southwest winds 30 to 40 mph with gusts up to 55 mph expected. * WHERE...Portions of south central and southwest New Mexico and southwest Texas. * WHEN...From 11 AM to 8 PM MST Wednesday. * IMPACTS...Gusty winds will blow around unsecured objects. Tree limbs could be blown down and a few power outages may result.

INSTRUCTION: Winds this strong can make driving difficult, especially for high profile vehicles. Use extra caution.

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Weather Topic: What is Evaporation?

Home - Education - Precipitation - Evaporation

Evaporation Next Topic: Fog

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

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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