
I am just not sure why, but something about the particularly strong 200mb wind flow just seem "off". I think more than anything, I just don't seem to recollect any recent past Spring seasons as having these winds so consistently spanning what seems like the entire Gulf region, across the Greater Antilles and Caribbean, and practically continuing almost all the way to Africa. Even during prior El Nino years we would see quite strong Westerlies, but strong as this upper shear seemed to be, those winds would moderate in intensity as that flow started exiting the Caribbean. I believe in those years with "El Nino" originating Westerlies, those winds would eventually interact with either an East Coast trough/TUTT condition, or maybe an oscillating mid-Atlantic trough that seemed persistently anchored in the W. Central Atlantic. Either way, even under those hostile upper air circumstances there would seem to be some downstream difluent conditions where those Westerlies eventually were shunted more pole-ward and an outflow channel would be created (if an active tropical wave were in the area to take advantage).
I very well realize that this is early May, but it just seems odd to me that the present upper level winds seem almost trapped within the sub-tropics latitudes and at present have nowhere else to go but as "East as far as the eye can see". More than likely this deviant flow will just give way to the eventual Easterly surge of ridging that would typically build Westward over the summer. Anyway you look at it though, I just cant see anything near term other than hostile wind shear conditions. These persistent upper air conditions do not look to change anytime in the foreseeable future. So if that were the case, it just wouldn't seem to matter what "alphabet soup" might be projected to surge in "our side of the bowl". These hostile conditions would seem to disrupt tropical genesis from occurring. While a late May or early June depression or even weak storm could well occur, I would bet against it at least until it was evident that some low latitude ridging was occurring somewhere.