Wthrman13 wrote:Extremeweatherguy wrote:thanks for that answer. So this may actually be a sign it is holding it's own?Wthrman13 wrote:The "feathery" appearance is the cirrus outflow from the storm. Notice how it is oriented radially outward from the center of the convection area? That indicates a large amount of upper-level divergence. There is still shear, but the convection is so intense that some of the outflow is fighting against it on the west side. The same thing happens in continental thunderstorms in regions of high shear; you can get what are called "backsheared" anvils that flow against the environmental winds at upper levels. It's one indication of an intense updraft.
Yes, the LLC, as far as I can tell, is just under the edge of the outflow from the convection on the NW side. So, it's holding it's own and may even be intensifying slightly at the time being. The shear ahead of it is still pretty robust, but has been decreasing steadily all day:
http://cimss.ssec.wisc.edu/tropic/real- ... g8sht.html
I'd say this has a pretty good chance of holding together.
So it could be pushing other weather away and as I have heard before, " creating it's own enviroment"?