Well, well well. I wonder what is causing the cut off lows to form in the eastern atlantic? All the models are forecasting anotherone to be stuck out there....
91L has about 24 hours to do something, it's firing up some modest convection near the LLC, but it's about to get pummeled by shear, so it's running out of time. It's odd, but by some definitions it's close to TD status, but probably will never get the benefit of the doubt, barring some very strong convection.
Former TD19 is just barely firing up any convection, but has still maintained a low level swirl around 41W 22N heading just south of due west.
How is Stan Stationary? I'm sure it's just a short term thing, but it still leaves me a little suprised.
The blob that is 92, it's way too complex for me to understand what's going on, though I still maintain there is a hint of a twist in the area near PR (perhaps it's simply convergence).
Any further thoughts and observations?
-------------------- M. S. Earth and Atmospheric Sciences, Georgia Tech - May 2020
NOAA MADIS/HADS Programmer
U. Arizona PhD Student
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