Panamanian Blob

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Stormavoider
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Panamanian Blob

#1 Postby Stormavoider » Wed Jul 26, 2006 5:58 pm

It seems to be trying to cross the isthmus. Is this too far south to become a Caribbean storm?

http://www.ssd.noaa.gov/goes/east/watl/loop-avn.html
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#2 Postby wxmann_91 » Wed Jul 26, 2006 6:00 pm

I noticed that too and I am almost certain that if it develops it will be an EPAC storm.
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#3 Postby CrazyC83 » Wed Jul 26, 2006 6:42 pm

More of an EPac worry than an Atlantic worry.
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#4 Postby gatorcane » Wed Jul 26, 2006 6:56 pm

CrazyC83 wrote:More of an EPac worry than an Atlantic worry.


I say EPAC 8-)
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#5 Postby Stormavoider » Wed Jul 26, 2006 6:58 pm

Has a system ever crossed over Panama and developed?
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Jim Cantore

#6 Postby Jim Cantore » Wed Jul 26, 2006 9:33 pm

Stormavoider wrote:Has a system ever crossed over Panama and developed?


Most likely, I cant name one though.
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#7 Postby HurricaneHunter914 » Wed Jul 26, 2006 9:58 pm

gatorcane wrote:
CrazyC83 wrote:More of an EPac worry than an Atlantic worry.


I say EPAC 8-)


Too bad, this is already making the cross over into the afterlife (Caribbean).
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#8 Postby senorpepr » Wed Jul 26, 2006 10:31 pm

The chances of this becoming a tropical cyclone (EPAC or Atlantic) are rather limited.

What you are witnessing is a typical Panama low associated with the Central American transitional monsoon.

Let me explain it...

There are three points in Central American where there is a break in the mountains that allows the Easterlies to easily cross over into the EPAC. Those three points are the Isthmus of Tehuantepec, Lake Nicaragua, and the Panama Canal Zone.

The Easterlies spill across these breaks whereas the rest of Central America finds the mountains and the inversion hindering the cross-over.

When the wind crosses over, the speeds increase. Shear associated with the speed convergence forces cyclone turning (and sometimes terrains helps this turning, which is the case for the Panama Low), which helps kick off three quasi-stationary lows in the aforementioned places.

In short, don't expect anything out of this blob. It's just our Panama low.
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#9 Postby wxmann_91 » Wed Jul 26, 2006 10:33 pm

senorpepr wrote:The chances of this becoming a tropical cyclone (EPAC or Atlantic) are rather limited.

What you are witnessing is a typical Panama low associated with the Central American transitional monsoon.

Let me explain it...

There are three points in Central American where there is a break in the mountains that allows the Easterlies to easily cross over into the EPAC. Those three points are the Isthmus of Tehuantepec, Lake Nicaragua, and the Panama Canal Zone.

The Easterlies spill across these breaks whereas the rest of Central America finds the mountains and the inversion hindering the cross-over.

When the wind crosses over, the speeds increase. Shear associated with the speed convergence forces cyclone turning (and sometimes terrains helps this turning, which is the case for the Panama Low), which helps kick off three quasi-stationary lows in the aforementioned places.

In short, don't expect anything out of this blob. It's just our Panama low.


I just learned something new today. Thanks senor 8-)
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Jim Cantore

#10 Postby Jim Cantore » Thu Jul 27, 2006 12:11 am

senorpepr wrote:The chances of this becoming a tropical cyclone (EPAC or Atlantic) are rather limited.

What you are witnessing is a typical Panama low associated with the Central American transitional monsoon.

Let me explain it...

There are three points in Central American where there is a break in the mountains that allows the Easterlies to easily cross over into the EPAC. Those three points are the Isthmus of Tehuantepec, Lake Nicaragua, and the Panama Canal Zone.

The Easterlies spill across these breaks whereas the rest of Central America finds the mountains and the inversion hindering the cross-over.

When the wind crosses over, the speeds increase. Shear associated with the speed convergence forces cyclone turning (and sometimes terrains helps this turning, which is the case for the Panama Low), which helps kick off three quasi-stationary lows in the aforementioned places.

In short, don't expect anything out of this blob. It's just our Panama low.


Good stuff, fact of the day 8-)
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#11 Postby mtm4319 » Thu Jul 27, 2006 1:28 am

I think the only time a TC hit Panama was in 1969...

Image
(click)
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#12 Postby Stormavoider » Thu Jul 27, 2006 7:59 am

It appears the bulk of the convection did cross into the Caribbean.
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#13 Postby HurricaneHunter914 » Thu Jul 27, 2006 11:44 am

http://www.nhc.noaa.gov/tafb_latest/atl ... BW_sm3.gif

In the next 3 days the NHC show a low pressure system in the Caribbean. Possible TD?
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#14 Postby Steve H. » Thu Jul 27, 2006 3:36 pm

Hah! And the at the 12z NAM LOL!!! :eek:
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#15 Postby Stormavoider » Thu Jul 27, 2006 5:10 pm

What is with the general clockwise rotation in this corner of the Caribbean? Is high pressure trying to build in?

http://www.ssd.noaa.gov/goes/east/watl/loop-avn.html
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