
Early start to the Cape Verde season?
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Early start to the Cape Verde season?
There is a very established wave exiting the continent of Africa at 1200 UTC. There even appears to be a decent mid-level rotation in the wave's axis. Though it is not unusual to have a strong wave exit this early in June, it is unusual how high in lattitude the 26ºC isotherm is in the eastern Atlantic for this time of year. If strong waves like this keep rolling off the west coast of Africa, fears of an early start to the 2005 Cape Verde season may be realized:


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Not quite yet I think guys.You have one ULL moving out to the NE and another approaching from the W.Then it is a little moisture out there as opposed to a couple of weeks ago just don't know if enough.
http://www.ssd.noaa.gov/PS/TROP/DATA/RT ... -loop.html
Off topic to this 10' rule in relation to tropical systems I need a memory refreshner Derek.
http://www.ssd.noaa.gov/PS/TROP/DATA/RT ... -loop.html
Off topic to this 10' rule in relation to tropical systems I need a memory refreshner Derek.
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Keep in mind, I was not trying to imply that this particular wave will develop into anything signficant in the context of my original post. Only that I have concerns the Atlantic Basin will experience Cape Verde storms earlier than the average year based on the fact the monsoon trough off of Africa is currently producing strong tropical waves (such as the one at present) and the 26ºC isotherm is at a higher lattitude near the Cape Verde Islands than what is typically observed this early in <b>June</b>. Obviously, the SAL might be a player in this too. A moderate-to-strong SAL could keep early Cape Verde activity in check. Though at present, the SAL seems to be extending east-to-west north of the MDR right now. Therefore, as of right now I would not be surprised if we observe cyclogenesis somewhere SE, S, or SW of the Cape Verdes during the next 3-6 weeks. Even the development of <b>2 or 3 storms before August 1st</b> in the MDR east of the Lesser Antilles would not shock me with the present oceanic heat content that is already there. See the image below:


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