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i know its in the warmest water in the  entire atlantic but would nor the slow movement cause upwelling?
OHC is very deep in that part of the Caribbean. The 26°C isotherm is over 100 meters of depth. It would take a multi-day stall before upwelling became a significant factor, and we're talking in terms of a Category 5 sustaining itself. For all practical purposes, the main reason even slow-moving hurricanes in the western Caribbean can maintain Cat 5 intensity well into November. Some of our most powerful historical Cat 5s were slow movers in that part of the world (Wilma, Mitch, etc.). It's where the Western Hemisphere's version of WPAC typhoons can occur, though still considerably rare.
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22 minutes ago, nycwinter said:

i know its in the warmest water in the  entire atlantic but would nor the slow movement cause upwelling?

It will cool the water at least slowly because it’s taking the potential energy from the warm ocean and converting it into kinetic energy (its a heat engine). That’s related to tropical cyclones redistributing heat to higher latitudes. That’s in addition to any cooling of the surface from upwelling. I believe these are two separate processes.

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Intense VHT is now going up in the NE eyewall. Obviously, we're in an ongoing rapid intensification phase. Expect some beefy pressure drops between now and Sunday afternoon with such an eyewall presentation on radar, which is getting more and more symmetrical each passing hour.

32b78a1df42ba5ea57a8af9c6c716ccd.gif

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This is exceptionally rapid organization. 

15z on 10/25
tUqRMDi.png

04z now, on 10/26
LhEdFyH.png
Fourteen hours between those two images is absolutely absurd. We kept harping that all forecast indicators were showing substantial decrease in wind shear to a near to pristine favorable upper environment. The system is now positioned right under an amplifying ULAC. Powder keg stuff. I think we'll see a Category 5 today.
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 This will be a great test to see how much cooling of the surface there is by 10/29. Here was the SST map as of 10/24: note the large area of 30-31C surrounding Jamaica, which is the warmest in the Atlantic basin:

IMG_4964.png.41dbe58c8d87e61ada35d444ff559322.png

 

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 This will be a great test to see how much cooling of the surface there is by 10/29. Here was the SST map as of 10/24: note the large area of 30-31C surrounding Jamaica, which is the warmest in the Atlantic basin:
IMG_4964.png.41dbe58c8d87e61ada35d444ff559322.png
 
Here's some heat content and isotherm depth maps as well. Melissa's core, despite being a slow-mover, has plenty of energy to tap prior to land interaction.

Credit to RSMAS at Miami for maintaining these to the public.

63aded4629ec72f629880c58cbe24066.gif


2032b35028d6942d2d1b4d729d24fc37.gif
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