Weather Alert in Texas
Special Weather Statement issued March 15 at 8:21PM 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: The strong cold front pushing across South Central Texas earlier this afternoon through this evening, brings a much cooler airmass across South Central Texas. Monday morning's lows over parts of the Hill Country and southern Edwards Plateau are expected to drop into the low to mid 30s with wind chills into the low to mid 20s. Temperatures into Tuesday morning will become even lower thanks to light winds and clearing high level cloud cover. This will lead to a light freeze across most of the Hill Country along with rural portions of the I-35 corridor and coastal plains and low- lying valleys. This cold episode could bring some challenges as growing season may have started over portions of the region. Therefore, we recommend to protect the four P's: Plants, People, Pets, and Pipes for the next few mornings. 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 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
Weather Topic: What is Graupel?
Home - Education - Precipitation - Graupel
Next Topic: Hail
Graupel is a form of precipitation that is created by atmospheric conditions
which cause supercooled water droplets to contact snow crystals and freeze to
their surface.
Sometimes known as soft hail or snow pellets, graupel is delicate and easily
destroyed by touch. Whereas hail usually falls during severe weather, graupel
doesn't require such conditions to form, and can form in mild precipitation
similar to situations which produce snowfall.
Next Topic: Hail
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