MESOSCALE DISCUSSION 0045 NWS STORM PREDICTION CENTER NORMAN OK 0226 PM CST SUN JAN 22 2012 AREAS AFFECTED...NERN TX...NRN LA...SRN/ERN AR...NWRN MS...WRN TN CONCERNING...SEVERE POTENTIAL...TORNADO WATCH LIKELY VALID 222026Z - 222230Z SEVERE THUNDERSTORMS SHOULD INITIATE BY EARLY EVENING NEAR THE ARKLATEX THEN RACE NEWD TOWARD WRN TN/NWRN MS AFTER DARK. DAMAGING WINDS AND ISOLATED TORNADOES ARE EXPECTED. A TORNADO WATCH WILL LIKELY BE REQUIRED BY 00Z. LEADING EDGE OF WELL DEFINED UPPER TROUGH IS ADVANCING ACROSS ERN OK/NERN TX AND WILL SOON OVERSPREAD THE LOWER MS VALLEY. IN ADVANCE OF THIS FEATURE...WARM MOIST BOUNDARY LAYER HAS SPREAD INTO SRN/ERN AR...AS NOTED BY SFC DEW POINTS RISING THROUGH THE UPPER 50S INTO THE 60S...WHILE A STUBBORN WEDGE OF COOLER AIR HAS YET TO BE DISPLACED OVER MUCH OF CNTRL/NWRN AR. CURRENT THINKING IS GREATEST AIRMASS DESTABILIZATION WILL OCCUR TO THE S-E OF THE AFOREMENTIONED WEDGE FRONT AND THIS WILL BE THE CORRIDOR OF GREATEST SEVERE THUNDERSTORM POTENTIAL. LATEST VIS IMAGERY DEPICTS AN INCREASING BAND OF LOW LEVEL CU ALONG THE DRY LINE NEAR I-35 OVER NCNTRL TX. THIS IS ALONG THE LEADING EDGE OF STEEPER LAPSE RATES AND IS CERTAINLY INDICATIVE OF STRONGER FORCING THAT WILL SOON OVERSPREAD THE ARKLATEX. WITH TIME THUNDERSTORMS COULD EVOLVE ALONG THIS LINE...OR PERHAPS EVEN DEVELOP WELL AHEAD OF THE WIND SHIFT WITHIN DEEPER CONFLUENT ZONE NEAR THE LA BORDER AS EXHIBITED BY SHOWERS BEGINNING TO DEEPEN FROM NEAR TYR TO JUST WEST OF SHV. NEEDLESS TO SAY VERY STRONG SHEAR WILL SUPPORT SUPERCELL DEVELOPMENT AND THE POTENTIAL FOR TORNADOES. ..DARROW.. 01/22/2012
This is a hazard specific graphic from the Storm Prediction Center. This graphic shows the potential for tornadoes this afternoon and tonight. The highest risk currently is centered from Little Rock, southeast to Jackson (MS), Northeast to Birmingham, and northwest to Jackson (TN). Within this area, residents have a 15% chance of experiencing a tornado within 25 miles of their location. When you think about those probabilities, they are actually pretty high. You have a nearly 1 in 5 chance of having a tornado occur within 25 miles of your location. Lower probabilities surround the 15% zone, but still present a substantial risk of tornadoes. In addition to the tornado risk, damaging winds will also be likely tonight. We’ll be providing live social media coverage all evening and overnight, so stay tuned!
Good afternoon,
I posted on the social media pages yesterday about how the mid-range models were showing a powerful upper level system moving through the Central United States later this weekend, and how it was pretty darn impossible to say anything with certainty. Even a day later, we’re still having that problem. I wanted to show you what kind of data we’re dealing with when it comes to this system.
This data comes from the Global Forecast System (GFS) and is from the 06Z run from early this morning. The first graphic shows the dewpoint output at 7 PM on Saturday. Notice that the dewpoints are fairly low along/ahead of the dryline across Texas with values from 50F to 54F. As a result of the low dewpoint values, instability is non-exsistant on this run. If this run were to verify, we would be lucky to get a rumble of thunder, with absolutely no severe weather to be found. Now, lets take a look at the same model except the 12Z version that was run later in the morning.
Now we fast forward to another model run from the GFS, the 12Z version run about 6 hours later. This is the same time period at 7 PM on Saturday with the same graphics as the 06Z run, except a few important differences. With the 12Z GFS, rich gulf moisture returns northward. 50F degree dewpoints are drawn northward along the cold front/dryline northward into Iowa. Dewpoints at/above 60 degrees spread inland across Texas and make it up to the Red River. Concentrating on Texas, notice how a 5 to 8 degree increase in dewpoints affects instability values. On the 06Z GFS with dewpoint values around 54F, there is no instability. With the 12Z run and with dewpoint values near 60-65F, a large instability pool is able to develop. Mixed Layer Instability is able to build up to 1000-1500 joules per kilogram (J/Kg). For a fall event in early November, that is a moderate to decently high amount of instability.
Here we’re looking at 500 MB (18,500 feet) winds and heights at 7 AM on Saturday from the 12Z GFS. While the instability/moisture questions remain, models are remaining fairly consistent on the position/strength of the upper level disturbance. Timing differences remain which would also have a significant impact on the forecast for the weekend, but the point I’m trying to make here is that this is a very powerful system. Winds at 500 MB exceed 80 to 100 knots. If moisture and instability are in place when this system arrives, there could be some severe weather issues. Even modest amounts of instability could do the job with this kind of a setup.
Can you understand why we can’t be specific yet on what we might be dealing with this weekend? We’ll be able to provide more details as we get closer to this possible event. Heck, it’s possible that there won’t be any event! We’re still over 125 hours away from this and high resolution model guidance doesn’t really kick in until 3 days out. Moisture return is a big question. The cold front that’s going to move through the region tomorrow night is going to really dry us out. Whether or not moisture can get back in here in time to produce any severe weather is the big question, as it normally is for fall/winter events. Stay tuned!
By roczag
By weatherworm