DTX "confidence higher than normal" due to consistency of GEFS/EPS at 500 mb
Attention during the coming days will be affixed on the mid latitude
cyclone/winter storm system that appears set to track through the
Lower Mississippi to Ohio River Valley Wednesday. Will not get into
details much since the storm system remains some 84 hours out,
rather will offer some commentary on the predictability of the
system. Definitely think its noteworthy to remark on the little to
no variability in the 500mb EOF patterns of the 22.12Z GEFS cluster
analysis. This lack of difference is between both eof1 and eof2 and
in the 500mb height difference signal at both Day3 and Day4. It is
also interesting, or maybe should not be surprising then, to not see
much d(prog)/dt variability in the 500mb vorticity field through
roughly the first 60 hours. Generally looking at a low variance,
strong closed off 500mb anomaly that digs clear through the Desert
SW into northern Mexico. Thereafter, variability does begin to
increase with the structure and timing of as many as 3 shortwave
centers that push into portions of western Canada, but do not see
much to suggest these vorticity anomalies will impact the phasing or
strengthening of the low pressure system as it tracks northeastward
out of the Lower Mississippi River Valley. Survey of 22.00Z EPS
member postage stamps is also suggestive of low solution variance.
The EPS members are showing a single mode characterized by heart of
cold side deformation/trowal impacting Lower Michigan (to varying
extents) with warm conveyor missing well to the south and east. What
will need to be sorted out is the quality and magnitude of moisture
that will advect meridionally into the system here locally rather
than just get shunted eastward. There are some indications in the
deterministic solutions that suggests convection and latent heating
over the Southeast United States could impact the low track. With
that stated, the forecasted structure and placement of the coupled
upper level jet into Ontario and Quebec supports a higher confidence
in a second low pressure center hanging close to Southeast Michigan
even if some east coast transfer wants to happen. Taking the lack of
solution variability in the EPS and GEFS in account, confidence is
higher than normal that the system will impact the area Wednesday
morning through Wednesday evening. The uncertainty is how far
northward the deformation snow will impact and what sort of snow
gradient will exist on the northern edge.