Weather Alert in Texas
Heat Advisory issued June 12 at 11:26PM MDT until June 17 at 12:00AM MDT by NWS El Paso Tx/Santa Teresa NM
AREAS AFFECTED: Eastern/Central El Paso County; Rio Grande Valley of Eastern El Paso/Western Hudspeth Counties; Rio Grande Valley of Eastern Hudspeth County
DESCRIPTION: * WHAT...For Friday, temperatures around 105. For Saturday through Monday, temperatures as high as 109. * WHERE...Eastern/Central El Paso County, Rio Grande Valley of Eastern El Paso/Western Hudspeth Counties, and Rio Grande Valley of Eastern Hudspeth County. * WHEN...From noon Friday to midnight MDT Monday Night. * IMPACTS...Hot temperatures may cause heat illnesses. * ADDITIONAL DETAILS...The hottest days will be Sunday and Monday with a low risk for highs at or above 110. The heat advisory will almost certainly need an areal expansion by Saturday or Sunday, and there is a low to moderate risk the heat advisory will need to continue for Tuesday.
INSTRUCTION: Drink plenty of fluids, stay in an air-conditioned room, stay out of the sun, and check up on relatives and neighbors. Take extra precautions when outside. Wear lightweight and loose fitting clothing. Try to limit strenuous activities to early morning or evening. Take action when you see symptoms of heat exhaustion and heat stroke.
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Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
Weather Topic: What are Altocumulus Clouds?
Home - Education - Cloud Types - Altocumulus Clouds
Next Topic: Altostratus Clouds
Similar to cirrocumulus clouds, altocumulus clouds are
characterized by cloud patches. They are distinguished by larger cloudlets
than cirrocumulus clouds but are still smaller than stratocumulus clouds.
Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km)
and may resemble, at times, the shape of a flying saucer.
These uncommon formations, called altocumulus lenticularis, are created by uplift
in the atmosphere and are most often seen in close proximity to mountains.
Next Topic: Altostratus Clouds
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