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West Pacific Tropical Action 2011


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They actually use 805mb relative vorticity as a proxy for max wind speed. I've never seen what the qualitative descriptions correspond to.

Ok, thanks. It was an empiric observation, where I have seen the "Intense" remark being forecasted when other guidance has near hurricane force winds. But with the description you give, it would highly depend on the size of the cyclone, surface translation of the wind, etc., so it makes quite a vague label with a varying correspondance to 1-min winds.

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I think this one is just born to be ugly...like ed mahmoud or hurricane igor

I'm wondering if this is the rare storm that hits Cat 4 without ever explosively intensifying (I know technically, it RI'd yesterday, but c'mon, that wasn't what any of us wanted to see)

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I'm wondering if this is the rare storm that hits Cat 4 without ever explosively intensifying (I know technically, it RI'd yesterday, but c'mon, that wasn't what any of us wanted to see)

That would be awfully boring. Anything below a cat 5 is unacceptable given that we are talking about the WPAC.

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I still think we should see this storm get to super-typhoon status... its just taking its sweet time, because its inner core took longer to form due to its large overall size.

That dry air to the north looks menacing, but the upper level flow really isn't letting that be advected into the circulation fully.

r9jtp0.gif

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Now I'm curious. At what level does Ma-On go from a cyclonic to anticyclonic circulation? I thought I had read somewhere that exceptionally strong cyclones can have a cyclonic circulation to a higher level (not sure if there is a corresponding increase in the height of the troposphere with that, or if a 'shorter' anticyclone just really cranks out the outflow).

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uhm, okay we have JMA upgrading the invest in the Philippine Sea into a TS...:arrowhead:

TS Tokage..

TS 1107 (TOKAGE)

Issued at 04:05 UTC, 15 July 2011line_menu.gif<Analyses at 15/03 UTC>Scale-Intensity-Center positionN14°05'(14.1°)

E132°55'(132.9°)Direction and speed of movementESE Slowly Central pressure1002hPaMaximum wind speed near the center18m/s(35kt)Maximum wind gust speed25m/s(50kt)Area of 30kt winds or moreS240km(130NM)

N130km(70NM)

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I don't know if there has ever been a study to confirm this (I'm short for time now but will search later), but I'm under the impression that larger tropical cyclones are more susceptible to dry air intrusions, mainly because their larger size gives the system a chance to sample a larger portion of the atmosphere, some of which might be dry air. In the latest TPW image... its hard to argue otherwise that dry air is not contributing to the degraded appearance of the system on microwave.

idetxd.png

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I got to read a UM Master's thesis, that theorized dry air did not substantially weaken well developed cyclones absent of shear. Of course, it was a master's thesis.

http://scholarlyrepository.miami.edu/cgi/viewcontent.cgi?article=1089&context=oa_theses&sei-redir=1#search=%22derek%20ortt%20masters%20miami%22

Semi-slow to load.

TC size and resistance to dry air, that sounds like something good for a graduate student to study...

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There's some northerly shear... weak to moderate maybe, but maybe just the kind that makes cyclones slowly intensify, or plateau when around major status... high end 4 or 5 requires almost perfect conditions.

llbQZ.gif

OTOH, if the upper ridge providing the shear moves little, then Ma-on would encounter less shear down the road.

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I got to read a UM Master's thesis, that theorized dry air did not substantially weaken well developed cyclones absent of shear. Of course, it was a master's thesis.

http://scholarlyrepository.miami.edu/cgi/viewcontent.cgi?article=1089&context=oa_theses&sei-redir=1#search=%22derek%20ortt%20masters%20miami%22

Semi-slow to load.

TC size and resistance to dry air, that sounds like something good for a graduate student to study...

Jason Dunion has also done some confirmation work that dry air absent shear is not a detriment to tropical cyclones.

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