Weather Alert in Texas
Special Weather Statement issued March 16 at 3:59PM CDT by NWS Austin/San Antonio TX
AREAS AFFECTED: Llano; Burnet; Williamson; Val Verde; Edwards; Real; Kerr; Bandera; Gillespie; Kendall; Blanco; Hays; Travis; Bastrop; Lee; Kinney; Uvalde; Medina; Bexar; Comal; Guadalupe; Caldwell; Fayette; Maverick; Zavala; Frio; Atascosa; Wilson; Karnes; Gonzales; De Witt; Lavaca; Dimmit
DESCRIPTION: A light freeze with low temperatures mainly between 30 and 32 degrees is forecast Tuesday morning for most of the Hill Country, as well as portions of the I-35 corridor and Coastal Plains, with the aid of light winds and clearing skies. A few of the lowest lying areas may briefly see temperatures of 27 to 30 degrees. Freezing temperatures may set in after midnight before all areas warm above freezing by about 9 AM Tuesday morning. This cold episode could bring challenges as the growing season may have started over portions of the region. Therefore, we recommend to protect Plants, People, and Pets. After Tuesday morning, expect warmer temperatures to prevail through the rest of the week.
INSTRUCTION: N/A
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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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