
East of Luzon, 14N 128E
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Typhoon Hunter wrote:Another invest pops up!
Shear is dropping a lot over the region whilst vorticity seems to be increasing:
http://cimss.ssec.wisc.edu/tropic2/real-time/windmain.php?&basin=westpac&sat=wgms&prod=vor&zoom=&time=
Steering environment seems pretty weak right now so I guess it won't be going anywhere too quickly. Given the low shear, boiling SSTs, upper level divergence it will be one to watch!
Typhoon10 wrote:Hey TH,
So for us amateurs trying to learn. I think you are saying Shear drop and vorticity increasing is both good for chance of systems to develop? But it could go anywhere?
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dexterlabio wrote:The shear east of 130 latitude is increasing, but the shear on the waters near the eastern side of the Philippines is pretty weak. By the way, I am basing my analysis to this chart: http://cimss.ssec.wisc.edu/tropic2/real-time/windmain.php?&basin=westpac&sat=wgms&prod=sht&zoom=&time=. If it takes more time to organize and strengthen on its current position before it moves somewhere else, then there is a high chance for it to develop. I agree with Typhoon Hunter, this is one invest to watch out for.![]()
Sorry for the ignorance, but what does upper level divergence contribute to the formation of tropical cyclones? Alll I know at this point are the shear's effect on a system, high STT's contributing to a system's consolidation and the steering environment affecting a system's movements, but I don't know much about this upper level divergence.Thanks.
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