
18z GFS...Landfall near Vero Beach... Huge difference is the vorticity is much more defined before Hispaniola and recovers quickly in the Bahamas compared to previous runs... IMO, GFS would strengthen Dorian more if it misses/brushes Hispaniola...
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SouthFLTropics wrote:I suppose the question of the day is "what is the new GFS seeing that everything else isn't"? Is it strictly the interaction with Hispaniola? Or is there more to it?
SouthFLTropics wrote:I suppose the question of the day is "what is the new GFS seeing that everything else isn't"? Is it strictly the interaction with Hispaniola? Or is there more to it?
TheStormExpert wrote:SouthFLTropics wrote:I suppose the question of the day is "what is the new GFS seeing that everything else isn't"? Is it strictly the interaction with Hispaniola? Or is there more to it?
It's weird to cause it is the model that sniffed Dorian out well before anyone else.
I think the models are picking up the slight erosion of the ridge temporarily by TD6 off of NC. That could be just enough to let it get the latitude before the ridge strengthens back and sends it west.
ScottNAtlanta wrote:I think the models are picking up the slight erosion of the ridge temporarily by TD6 off of NC. That could be just enough to let it get the latitude before the ridge strengthens back and sends it west
Nederlander wrote:First, a disclaimer: I understand that you shouldn’t focus on the center of the NHC cone.
That being said, IF Dorian travels the center of the NHC come, then land interaction would be pretty minimal as it splits PR and Hisp. Therefore, the weakening to TS and staying there is curious. Maybe just a conservative estimate until there’s a better idea of how land interaction will affect Dorian?
BobHarlem wrote:18z HMON and 18z HWRF both go poof. And dissipate the system. HWRF before it even reaches Hispaniola.
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