Adam Atkins
EF2
Tomorrow
I couldn't be happier with the 6Z day one SPC outlook. Why? It means less chasers will be out in the I40 W domain. I have a feeling most people use the SPC's outlook as their primary chase tool, which is intelligent and useful, but in this case, it seems their preoccupied with other things. They fail to mention anything about the veered mid/upper level flow near the base of the shortwave trough.
Unfortunately I don't see any large scale subsidence to clear out the deep moisture ahead of the dryline, and as Snyder said, it could be a very skinny CAPE axis, which from my experience, SUCKS for chasing. I'd equate it to a rollercoaster ride, up and down (storms).
I'm banking on the possibility of isolated convection due to upper level convergence in the right exit region of the jet. The more isolated the storms, the better the chasing, however, as previous research has shown, outflow boundaries locally increase the helicity and CAPE, leading to the formation of tornadoes.
Tornado potential definitely increases through the late afternoon, early evening when moisture increases and mid-level flow becomes more veered.
Sunday looks like a heavyweight match between storms, so I'm chasing tomorrow.
I couldn't be happier with the 6Z day one SPC outlook. Why? It means less chasers will be out in the I40 W domain. I have a feeling most people use the SPC's outlook as their primary chase tool, which is intelligent and useful, but in this case, it seems their preoccupied with other things. They fail to mention anything about the veered mid/upper level flow near the base of the shortwave trough.
Unfortunately I don't see any large scale subsidence to clear out the deep moisture ahead of the dryline, and as Snyder said, it could be a very skinny CAPE axis, which from my experience, SUCKS for chasing. I'd equate it to a rollercoaster ride, up and down (storms).
I'm banking on the possibility of isolated convection due to upper level convergence in the right exit region of the jet. The more isolated the storms, the better the chasing, however, as previous research has shown, outflow boundaries locally increase the helicity and CAPE, leading to the formation of tornadoes.
Tornado potential definitely increases through the late afternoon, early evening when moisture increases and mid-level flow becomes more veered.
Sunday looks like a heavyweight match between storms, so I'm chasing tomorrow.