Mikey Gribble
EF5
Just going to copy and paste the latest post I made on my blog. I have a map on there too if you're interested (blog link is in my signature). Basically I am liking the OKC area as a starting point. Everything seems to be on track for a good tornado threat tomorrow. Below is pasted from my blog...
The going forecast seems on track. The only notable change with the 12Z runs of the NAM and GFS are that both models made a very subtle move towards the other solution on 850mb winds. The GFS isn’t veering them quite as bad and the NAM is veering them slightly more, so I still think what will actually happen is 850mb winds will veer slightly immediately ahead of the dryline and then back 50 miles or so off the boundary. That will work out just fine.
Aside from the difference with 850mb winds and the GFS being slightly more progressive, the only other major difference between the two models remains the extent of surface heating and resultant CAPE. The NAM continues to be more aggressive with surface heating with temps across the Oklahoma portion of the warm sector in the mid to upper 70′s by 00Z. The GFS keeps surface temps about 10 degrees cooler. As a result the GFS has CAPE <2000 across Oklahoma and the NAM has it >2000 all across Oklahoma and even approaching 3000.
The cause of the temperature/CAPE difference between the models appears to be a result of the GFS keeping the warm sector sacked in with low level clouds through the day while the NAM begins breaking up the low level clouds and allows for partial clearing by early afternoon. This is very apparent if you compare the two models 850mb RH charts through the day.
I am thinking the NAM is correct and we will get partial clearing and good insolation during the afternoon. The GFS seems to over forecast the extent of low level clouds on a fairly regular basis. Plus the NAM typically does a decent job forecasting CAPE.
Both models are about on the same page with moisture return. They both have low 60 dewpoints nosing into Kansas by late afternoon with low to mid 60′s across Oklahoma. 60 degree dewpoints are just now nosing on shore in south Texas, so I’m still a little worried about that verifying, but even if moisture was slightly worse than forecast it wouldn’t be a big deal. There is room to spare with dewpoint spreads and LCL’s will be sufficiently low for a good tornado threat so the moisture question is inconsequential at this point IMO.
So basically everything is coming together quite nicely for a few tornadic supercells tomorrow. I am worried about the extent of forcing for a squall line over the northern portion of the dryline, but as you go south along the dryline storms will be more discrete, so again not a real issue.
I think the best compromise of expected convective evolution(mode), CAPE and shear is all setting up across central Oklahoma. I expect the best tornadic storms to fire along the dryline between Kingfisher and Ardmore Oklahoma. I plan on heading to just north of OKC tomorrow morning and I will fine tune the forecast from there and adjust as needed.
I expect at least a couple cyclic tornadic supercells to come off the dryline tomorrow. Any storms firing along the dryline in the area I mentioned above will pose a threat for a strong tornado or two as they move downstream into the northeast and east central portion of Oklahoma later in the day. I’d put the absolute highest tornado probability over the southern half of SPC’s moderate risk area in the latest Day 2 outlook.
The going forecast seems on track. The only notable change with the 12Z runs of the NAM and GFS are that both models made a very subtle move towards the other solution on 850mb winds. The GFS isn’t veering them quite as bad and the NAM is veering them slightly more, so I still think what will actually happen is 850mb winds will veer slightly immediately ahead of the dryline and then back 50 miles or so off the boundary. That will work out just fine.
Aside from the difference with 850mb winds and the GFS being slightly more progressive, the only other major difference between the two models remains the extent of surface heating and resultant CAPE. The NAM continues to be more aggressive with surface heating with temps across the Oklahoma portion of the warm sector in the mid to upper 70′s by 00Z. The GFS keeps surface temps about 10 degrees cooler. As a result the GFS has CAPE <2000 across Oklahoma and the NAM has it >2000 all across Oklahoma and even approaching 3000.
The cause of the temperature/CAPE difference between the models appears to be a result of the GFS keeping the warm sector sacked in with low level clouds through the day while the NAM begins breaking up the low level clouds and allows for partial clearing by early afternoon. This is very apparent if you compare the two models 850mb RH charts through the day.
I am thinking the NAM is correct and we will get partial clearing and good insolation during the afternoon. The GFS seems to over forecast the extent of low level clouds on a fairly regular basis. Plus the NAM typically does a decent job forecasting CAPE.
Both models are about on the same page with moisture return. They both have low 60 dewpoints nosing into Kansas by late afternoon with low to mid 60′s across Oklahoma. 60 degree dewpoints are just now nosing on shore in south Texas, so I’m still a little worried about that verifying, but even if moisture was slightly worse than forecast it wouldn’t be a big deal. There is room to spare with dewpoint spreads and LCL’s will be sufficiently low for a good tornado threat so the moisture question is inconsequential at this point IMO.
So basically everything is coming together quite nicely for a few tornadic supercells tomorrow. I am worried about the extent of forcing for a squall line over the northern portion of the dryline, but as you go south along the dryline storms will be more discrete, so again not a real issue.
I think the best compromise of expected convective evolution(mode), CAPE and shear is all setting up across central Oklahoma. I expect the best tornadic storms to fire along the dryline between Kingfisher and Ardmore Oklahoma. I plan on heading to just north of OKC tomorrow morning and I will fine tune the forecast from there and adjust as needed.
I expect at least a couple cyclic tornadic supercells to come off the dryline tomorrow. Any storms firing along the dryline in the area I mentioned above will pose a threat for a strong tornado or two as they move downstream into the northeast and east central portion of Oklahoma later in the day. I’d put the absolute highest tornado probability over the southern half of SPC’s moderate risk area in the latest Day 2 outlook.