windstorm99 wrote:There are baroclinic signatures present so this systems identity in my opinion is up for question...I say more under sub-tropical TD for now.
Upper level winds will have to put in there part first.
The system is becoming tropical based on fsu core data. Yes it is not intensely warm core but becoming so. Also durning the latest satellite shows that that feeder band/trough boundry that was hanging from the south, is now starting to wash out. Over all the area of convection appears to be mostly formed by tropical means. Do I think this could have some extratropical/baroclinic things to it, to a point. But you can say that for Barry,Alison,Arlene,Alberto, and a long line of systems. Really we will know more when the recon gets into the system...It could be soildly warm core like the recon found for Barry. Shear stops develop but it does not stop it from being a tropical cyclone. Once the ridge forms to the north,,,and the cyclone moves under it, watch for the shear to decrease.
Can't wait for recon....
Also the high could be building at the surface. Stopping the cyclone/LLC. But at the upper levels the eastward movement of convection is still occuring. The high has to build upwards through the Atmosphere to catch the convection. Yes there is shear.