Alright, let's get down to it. There are many concerns regarding Erika becoming a hurricane before landfall ... those concerns are well-warranted. Many parameters are being met for rapid intensification once the LLC becomes well-defined (which shouldn't take very long). RECON data just obtained at 26.6ºN, 85.4ºW obtained flight level winds (1500 ft) of 48.3 mph and a 1008 mb pressure.
1) High Oceanic Heat Content - SST's are in the 31-32ºC range.
2) Upper high over Erika allowing for good ventilation of the system ... particularly with the equatorial outflow channel, enhanced by a weakening ULL to its SSE in the Western Caribbean Sea.
3 Single-channel Outflow (on the equatorial side). The single-channel outflow may be divided into two subcategories based on direction of the outflow channel. Tropical cyclones with single-channel poleward outflow pattern generally intensify at an average maximum rate of 15 to 20 kt/6 hr. Tropical cyclones with single-channel equatorward outflow pattern generally intensify at an average maximum rate of 25 to 28 kt/6 hr. Dual-channel Outflow. Tropical cyclones with a dual-channel outflow pattern generally intensify at an average maximum rate of 35 kt/6 hr.
4) Cumulus Convection - The cumulus convection is increasing.
5) Weak Vertical Wind Shear
The SST's across the Gulf and across the expected path of Erika will remain anywhere between 30ºC-32ºC, plenty warm to support and allow for Erika to strength given the high SST's. However, there's a fly in the ointment, the SST's left in the wake of Claudette ... though not apparent on actual SST's, it is apparent deeper down where the waters were upwelled...
Sea-Surface Temperatures

Second Look

SST-Depth

Heat Content

Usually, with rapid intensification parameters involving SST's, usually you would need a sufficient deep layer of warm water (usually about 50m deep).
Otherwise, Erika should become a hurricane because there are many, many solid factors going with it ...
SF