Bill Schintler
EF4
Chase target:
10 miles E. of Merriman, NE on US 20 (50 miles W. of Valentine).
Timing:
Storm initiation 6 PM CDT.
Comments:
Isolated high-based supercells between 7 and 9 PM, with an evolution into a multicell complex with an impressive lightning show after sunset.
Discussion:
00Z H7 UA analysis indicates digging trough in the WRN US while two shortwaves are approaching the Pacific coast. Forcing provided by the second of these two waves will provide the dynamics for SFC cyclogenesis in NERN CO tomorrow afternoon. A SFC boundary trailing NE from this low will provide the focus for SVR WX as a narrow axis of moisture is advected NW along and just NE of the boundary along upsloping terrain.
This evening, 00Z NAM initialized slightly cool with regard to SFC temps while the observed dryline position was 80mi E of the NAM solution, no doubt due to the model's lack of resolution with the shallow moisture layer which mixed out rapidly. This evening's NAM is very similar to the 12Z run with regard to SFC moisture, temperatures, and QPF for tomorrows 00Z FCST. Even after adjusting the position of the WWRD extent of the moisture to the E and NE, sufficient moisture with a dewpoint of 50F (the target elevation is just under 3000ft) should be in place at the target area. 12Z models (NAM, GFS, UKMET, and NGM) differed somewhat as to the placement of the SFC features, with the NAM and GFS in good agreement with low strength and location. Of those two, the GFS (which has been performing best lately for QPF), delays precipitation onset and places it 30 miles further to the north and west. The UKMET and NAM are both in good agreement with QPF while the UKMET is 70 mi northeast of the NAM with the location of the low. The NGM is the outlier with all parameters and will be discounted.
Adequate instability, with both SBCAPEs and 100mb MLCAPEs of around 1000J/kg, will couple with good shear parameters. A 55kt H5 streak on top of 15kt ERLY SFC flow should result in deep-layer shear to 60kts. Hodograph curves are somewhat of a question, however. Depending on relationship between the speed gradient on the NRN edge of the H85 and H7 jets, SFC-3km SRH's should locally reach 200m^2/s^2. Two FCST concerns relate to the possibility of excessive dry air advection into the target area. the first is the possibility that the DL will advance too far to the NW of the best SFC-H7 flow. The second concern is dry air entrainment into the updrafts, however, it appears as though H7 relative humidities should remain above 50% to the NW of the SFC boundary. A 70kt LLJ will sustain the storm complex as it moves to the E at 30 mph overnight.
- bill
10 miles E. of Merriman, NE on US 20 (50 miles W. of Valentine).
Timing:
Storm initiation 6 PM CDT.
Comments:
Isolated high-based supercells between 7 and 9 PM, with an evolution into a multicell complex with an impressive lightning show after sunset.
Discussion:
00Z H7 UA analysis indicates digging trough in the WRN US while two shortwaves are approaching the Pacific coast. Forcing provided by the second of these two waves will provide the dynamics for SFC cyclogenesis in NERN CO tomorrow afternoon. A SFC boundary trailing NE from this low will provide the focus for SVR WX as a narrow axis of moisture is advected NW along and just NE of the boundary along upsloping terrain.
This evening, 00Z NAM initialized slightly cool with regard to SFC temps while the observed dryline position was 80mi E of the NAM solution, no doubt due to the model's lack of resolution with the shallow moisture layer which mixed out rapidly. This evening's NAM is very similar to the 12Z run with regard to SFC moisture, temperatures, and QPF for tomorrows 00Z FCST. Even after adjusting the position of the WWRD extent of the moisture to the E and NE, sufficient moisture with a dewpoint of 50F (the target elevation is just under 3000ft) should be in place at the target area. 12Z models (NAM, GFS, UKMET, and NGM) differed somewhat as to the placement of the SFC features, with the NAM and GFS in good agreement with low strength and location. Of those two, the GFS (which has been performing best lately for QPF), delays precipitation onset and places it 30 miles further to the north and west. The UKMET and NAM are both in good agreement with QPF while the UKMET is 70 mi northeast of the NAM with the location of the low. The NGM is the outlier with all parameters and will be discounted.
Adequate instability, with both SBCAPEs and 100mb MLCAPEs of around 1000J/kg, will couple with good shear parameters. A 55kt H5 streak on top of 15kt ERLY SFC flow should result in deep-layer shear to 60kts. Hodograph curves are somewhat of a question, however. Depending on relationship between the speed gradient on the NRN edge of the H85 and H7 jets, SFC-3km SRH's should locally reach 200m^2/s^2. Two FCST concerns relate to the possibility of excessive dry air advection into the target area. the first is the possibility that the DL will advance too far to the NW of the best SFC-H7 flow. The second concern is dry air entrainment into the updrafts, however, it appears as though H7 relative humidities should remain above 50% to the NW of the SFC boundary. A 70kt LLJ will sustain the storm complex as it moves to the E at 30 mph overnight.
- bill