NDG wrote:I just went back through the last 10 days, the windshear axis across the eastern Caribbean has been present just about every day, I never bought the idea from the models that the shear axis is going to move out of the way as Danny approaches the Islands.
That's the semi-permanent mid oceanic trough. It's an the upper tropospheric feature (hence, why it's call the TUTT), and it's position and strength both do fluctuate. On occasion, as I alluded to in a post from a few days ago, pieces of vorticity fracture off of the trough, and generally retrograde toward the W or SW. Its evolution over the course of a season is pretty fascinating to watch on water vapor imagery, especially with vapor-derived winds overlaid.