The low level vorticity at 850 mb is very weak in the vicinity of the convection. The main vorticity lobe is situated farther south, and it has been weakening. There is a high amplitude
low level moisture surge in the area, but convergence is essentially non-existent. All of the convection is attributable to the well defined
divergence (varying wind speeds among heights) in the area. Without substantial convergence/LL vorticity, this system will not have an opportunity for development. The projected favorable environment, represented by a well defined 250 mb anticyclone, also indicates the absence of any defined forcing for convection. The ECMWF and GFS do not develop a closed low/sfc reflection as the system passes through the Lesser Antilles. Only the unreliable NAM develops a sfc low. Thus, I don't envision any significant development with this system. Furthermore, any land interaction with Puerto Rico/Hispaniola would affect any remnant vorticity lobes.