BensonTCwatcher wrote:Hmm seeing a LOT of confident statements in the blocking ridge setup, and I am not stating that that in any way that scenario is not the most likely one at this time. But own personal observations of many other synoptic scale setups 100 hours or more in the future has something nagging at me.
1. The "thumb" portion of the ridge that will be in place SW of Bermuda with the East/West axis is clearly the dominant steering feature ( sown on GFS 500 mb height)
2. I see in the GFS model upstream sampling (soundings) ahead of the storm the steering flow at 102 hours is WNW up through 500 mb height
3. I also notice the flow is much more northerly both above 500 mb AND as you go up the FL east coast. There does not seem to be any wiggle room either. I see that if this storm is stronger than forecast at 102 hours, or if it is riding the right side of the forecast envelope it could be influenced by the change in the steering vector right at the "thumbnail" portion of the clockwise flow - somewhere around WPB.
4. The above factors combined with the angle of the FL coast makes a FL landfall point forecast slip up the coast as it approaches. Given we are still pretty far out from this point, I can see at least a possibility that this "misses the 2 a.m. Monday forecast point by being much stronger than a TS and being a tad on the right of the guidance. There are ensemble members showing this on the latest run. Not at all saying this re-curves OTS or anything like that, or even that this does not get into the Gulf - still most likely- just that clearly the intensity forecast confidence is low and if this at all a strong hurricane coming through the Bahamas it looks like the steering flow will be quite different. Some Dominoes stacked up here on this one. Won't be sure which way they will fall till the wee hours on Monday though.
Regarding the upcoming 500-mb synoptic setup: there is a striking similarity between the ensemble projections and the analysed setup for Matthew (2016) in terms of the orientation, position, and amplitude of the Western Atlantic Ridge (WAR). (Additionally, note that
several models have shifted eastward since
06Z, a few of which even show some eastward component by the end of the period.) Note that the 590-dm contour forms a parabolic, SSE-to-NNE curve near the longitude of West Palm Beach or slightly eastward. If TD Thirteen is a strong (that is, deep) Category-4+ TC as it nears and passes through the Bahamas, then it is likely to sense the western edge of this contour, since such a strong system would easily reach the highest of the mid-levels. So at this point I will continue to give 60/40 advantage to the likelihood that TD Thirteen, while attaining major-hurricane status, will curve between FL and Grand Bahama, narrowly missing FL to the east, à la Matthew (2016). Unfortunately, the Bahamas will very likely experience a devastating hurricane, particularly the central and northwestern Bahamas, including New Providence, the site of the capital Nassau, and Grand Bahama. Those areas would likely experience the northeastern portion of the RMW. If the ridge were stronger and farther NW I would put the risk to South Florida at a much higher level of likelihood.
06Z GEFS00Z EPSMatthew (2016)Mean climatological path (August)