Aric Dunn wrote:Also the convection building to the NW is not directly associated with Colin.. however it provide a better assessment of the environment ahead of colin.. clearly some more moisture exists and better divergence aloft although its a very narrow area it is possible to see a slight improvement especially if it were to slow down some..
These are excellent and important points. Colin's weak (open?) circulation is indeed no longer seriously capable of producing significant convection, compared to what is occurring with the larger synoptic scale lift on the divergent east side of the large upper trough to it's NW. Until the environment gets better for Colin (or, more likely, what will be it's remnants), I think we're probably back to looking for signs of a center regenerating along a wave axis for the next few days.