98L is far from unworthy to discussion... There is a potent little vortex relative to what convection is occasionally fighting shear in the SW quadrant. When the shear relaxes, this system may very well lurch into a development phase... Said shear is still modeled to relax, and, the system its self is moving slowly west and away from the axis of upper level easterlies.

But, agreed, the system off the SE U.S. Coast is an important feature to monitor. I have put together an entry and placed it over in the 2007 Storm Forum. It does not say anything spectacular but is an attempt really to raise awareness and discuss some factors that may lead to development.