cheezyWXguy wrote:Shuriken wrote:Blinhart wrote:But the question is what are the hostile conditions that the MODELS are seeing that none of us (not even the NHC) are seeing???
Right now all we see in the foreseeable future are high SSTs and light shear, so what is it????????
I would guess high-altitude cap -- the "heat bulge" is still pretty thick in early August; and a storm which cannot effectively vent at 250-200mb will just putter along as a TD/TS through thousands of miles of otherwise favorable conditions.
Actually high pressure at that height would be preferred for intensification. Often one of the things we hear about most in rapidly strengthening storms is their positions under upper level "anticyclones" or areas of high pressure. Low pressure systems at that level are usually responsible for weakening tropical systems by shearing them out and restricting outflow.
An anticyclone aloft is certainly conducive, but, IMO, it's not the critical factor. I have watched a LOT of early-season whirls find themselves in ideal conditions near the Caribbean, but still refuse to develop. In contrast, I have seen storms in mediocre low/mid-level environments power up due to being able to effectively "clear the pipe" all the way to 70,000ft -- Hurricane Gustav is the arch-typrical example here: a storm which went from TS to 150 in less that 48hrs despite strong southwesterly shear in the mid-layers, catching everyone with their pants down.
Earnesto is clearly having trouble in this regard -- a good sized system with a well-developed LLC , but no really cold cloud-tops. If it doesn't develop a bright red meatball on the Rainbow IR tonight, my hunch is it'll be weaker tomorrow that it is today.