Bill Schintler
EF4
Chase target for Monday, January 7
Chase target:
Sallisaw, OK (along I-40, 13 miles west of Fort Smith, AR).
Timing and storm mode:
Convection will be ongoing and reach the target area at 3 PM, CST. A few low-topped supercells may be embedded within the larger convective mass, and a few weak tornadoes cannot be ruled out. Storm motion will be rapid, with individual cells lifting off to the northeast at 40 mph. Because of the rapid storm motion, poor terrain, and embedded nature of any storm structure, it will be a poor chase day.
Synopsis:
UA analysis indicates several disturbances embedded within the WRN CONUS trough, with a lead S/WV over ERN NM and a couple of disturbances lifting through CA. Upstream soundings (FWD, MAF, AMA, and EPZ) indicate steep lapse rates below 600mb. SFC dewpoints have increased to 55F in most of SERN OK, while a 100-150mb deep moist layer is indicated in ERN TX per soundings and the visible satellite loop. Models have initialized a few degrees too low on LLVL dewpoints.
Discussion:
Overnight, differential advection of the aforementioned moisture and EML should be maximized over ERN OK and SWRN AR. Convection should fire by late morning in the warm sector and well E of the significant SFC features in a zone of strong WAA in the H8-H9 layer. During the mid-day hours, a few breaks in the ST deck should allow for weak heating and a narrow axis of SFC-based instability should develop along the OK/AR border by early afternoon.
Marginal instability will be collocated with impressive shear parameters. MLCAPE’s should reach 1000J/kg with a 100mb deep moist layer and SFC dewpoints AOA 60F, despite poor lapse rates above 600mb. Most of the CAPE should be concentrated in the 900mb-600mb layer. Deep layer shear will exceed 60 kts as 70kt H5 flow overspreads the area. In ECNTRL OK, SFC winds should locally back which will enhance SFC-2km hodograph curvatures as the entrance region of a 35kt H9 LLJ overspreads the area. Low SFC dewpoint spreads in the neighborhood of 5F will contribute towards LCL levels around 700m AGL, resulting in an enhanced tornado threat given a healthy amount of directional shear in that layer.
- bill
[FONT="]9:10 PM CST, 01/06/08[/FONT]
Chase target:
Sallisaw, OK (along I-40, 13 miles west of Fort Smith, AR).
Timing and storm mode:
Convection will be ongoing and reach the target area at 3 PM, CST. A few low-topped supercells may be embedded within the larger convective mass, and a few weak tornadoes cannot be ruled out. Storm motion will be rapid, with individual cells lifting off to the northeast at 40 mph. Because of the rapid storm motion, poor terrain, and embedded nature of any storm structure, it will be a poor chase day.
Synopsis:
UA analysis indicates several disturbances embedded within the WRN CONUS trough, with a lead S/WV over ERN NM and a couple of disturbances lifting through CA. Upstream soundings (FWD, MAF, AMA, and EPZ) indicate steep lapse rates below 600mb. SFC dewpoints have increased to 55F in most of SERN OK, while a 100-150mb deep moist layer is indicated in ERN TX per soundings and the visible satellite loop. Models have initialized a few degrees too low on LLVL dewpoints.
Discussion:
Overnight, differential advection of the aforementioned moisture and EML should be maximized over ERN OK and SWRN AR. Convection should fire by late morning in the warm sector and well E of the significant SFC features in a zone of strong WAA in the H8-H9 layer. During the mid-day hours, a few breaks in the ST deck should allow for weak heating and a narrow axis of SFC-based instability should develop along the OK/AR border by early afternoon.
Marginal instability will be collocated with impressive shear parameters. MLCAPE’s should reach 1000J/kg with a 100mb deep moist layer and SFC dewpoints AOA 60F, despite poor lapse rates above 600mb. Most of the CAPE should be concentrated in the 900mb-600mb layer. Deep layer shear will exceed 60 kts as 70kt H5 flow overspreads the area. In ECNTRL OK, SFC winds should locally back which will enhance SFC-2km hodograph curvatures as the entrance region of a 35kt H9 LLJ overspreads the area. Low SFC dewpoint spreads in the neighborhood of 5F will contribute towards LCL levels around 700m AGL, resulting in an enhanced tornado threat given a healthy amount of directional shear in that layer.
- bill
[FONT="]9:10 PM CST, 01/06/08[/FONT]
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