
Low forming east of bahamas!
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I showed in this another thread. It's on the floater.
http://www.ssd.noaa.gov/PS/TROP/DATA/RT ... -loop.html
http://www.ssd.noaa.gov/PS/TROP/DATA/RT ... -loop.html
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- Hurricanehink
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margaritabeach
- Tropical Depression

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TWOAT
TROPICAL WEATHER OUTLOOK
NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL
530 PM EDT THU JUN 16 2005
FOR THE NORTH ATLANTIC...CARIBBEAN SEA AND THE GULF OF MEXICO...
AN AREA OF DISTURBED WEATHER HAS DEVELOPED ABOUT MIDWAY BETWEEN THE
BAHAMAS AND BERMUDA. THIS SYSTEM IS CURRENTLY POORLY ORGANIZED.
HOWEVER...SOME SLOW DEVELOPMENT IS POSSIBLE OVER THE NEXT DAY OR
TWO AS IT MOVES NORTHEASTWARD.
TROPICAL WEATHER OUTLOOK
NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL
530 PM EDT THU JUN 16 2005
FOR THE NORTH ATLANTIC...CARIBBEAN SEA AND THE GULF OF MEXICO...
AN AREA OF DISTURBED WEATHER HAS DEVELOPED ABOUT MIDWAY BETWEEN THE
BAHAMAS AND BERMUDA. THIS SYSTEM IS CURRENTLY POORLY ORGANIZED.
HOWEVER...SOME SLOW DEVELOPMENT IS POSSIBLE OVER THE NEXT DAY OR
TWO AS IT MOVES NORTHEASTWARD.
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- cycloneye
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My take about the area of concern in this thread is that the upper flow will cause the area to move progressivly to the NE going away from the warm waters that it is now to the fishes and cooler sst's.Also It is embedded to the TUTT trough located in the western atlantic and that is not favorable for development.The only way that this disturbance can develop is for it to remain in the above 80*F waters and detach itself from the TUTT trough.If this doesn't form into something I think that it will be a while that we will not see Bret somewhere so the waiting game would be longer.
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Matt-hurricanewatcher
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Derek Ortt
cyc,
these types of TC's can easily develop over 70F SST.
SST does not in any way affect intensity change (except for providing extra moisture, allowing for a storm to become a major hurricane). It is the temperature difference between the SST and the upper air temps that determines if a TC can form and intensify in the TS and cat 1-2 stage (via the instability parameters). These troughs have colder air aloft; thus, they can develop over very cool waters
these types of TC's can easily develop over 70F SST.
SST does not in any way affect intensity change (except for providing extra moisture, allowing for a storm to become a major hurricane). It is the temperature difference between the SST and the upper air temps that determines if a TC can form and intensify in the TS and cat 1-2 stage (via the instability parameters). These troughs have colder air aloft; thus, they can develop over very cool waters
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- george_r_1961
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Good point Derek. Until recently I always believed it was a hard and fast rule that SST's be above 80 for development to occur. Its the instability caused by the temperature differences between the surface layer and the upper layers that cause cionvection. Add favorable upper winds and preferably an upper level high and you have a tropical cyclone.
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Matt-hurricanewatcher
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