Despite
southeasterly winds, it cooled down to 67F before low clouds came in
last night, going below some model guidance unlike most recent nights.
The low clouds quickly broke up, with a rapid warmup to a high of 91F
and a maximum wind of at least 22 kt. However, mid to upper-level clouds
could have tempered the warmup slightly. Day 12 will overall be
substantially cloudier than the past 2 weeks. A surface low-pressure
approaching from the west will lead to stronger and deeper moisture
advection from the Gulf of Mexico tonight with southeasterly winds,
leading to a warmer low than we’ve seen in the past 2 weeks, likely near
or above most model guidance. However, I am hesitant to go too warm
after last night’s surprise low. Also, there’s still some uncertainty of
timing and thickness of the low clouds, with HRRR not becoming overcast
until 12z, and not very thick, while NAM 3-km shows thickening low
clouds by 03z. Reality will probably be in between. There will also be
some mid to high-level clouds that could hamper cooling regardless of
the low-level clouds.
How much the clouds break up tomorrow is also highly uncertain, with
HRRR quickly clearing out the low-level clouds, leading to a hotter
high, while the NAM 3-km has the clouds persisting for most of the day,
leading to a cooler high. There’s even a positive feedback making it
especially tricky, since any sunshine will help heat up the ground,
helping to burn off the low clouds faster, etc. Even if the low clouds
clear out, mid to upper-level clouds will remain to temper the warmup,
and HRRR tends to warm it up too much with these clouds. Still, there
may be enough heat and low-level moisture for scattered showers to occur
along a subtle pre-frontal trough/low-level convergence zone in the
vicinity, though models indicate very few and weak storms if any at all
in the vicinity, with the strong forcing with the real cold front still
staying to the northwest.
The greater cloud cover could also inhibit winds slightly, making it
more difficult to mix stronger winds aloft down to the surface. Any
showers that do form tomorrow afternoon could briefly increase winds
somewhat but they do not look nearly deep enough to produce strong cold
pools with strong gust fronts like along the real cold front to the
northwest. All models agree that the main squall line associated with
the cold front will still be at least 100 miles (160 km) to then
northwest of San Antonio even at the end of the period (Sunday 06z),
which means that even if the cold front and squall line advance more
quickly to the southeast than modeled, which sometimes happens, it is
still unlikely to reach San Antonio in time to affect day 12.
| Source: PivotalWeather |
| Source: PivotalWeather |
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