All the possible fictitious forces pertain to this problem, which is partly what makes going to the E-frame difficult. There is a linear fictitious force parallel to the incline just because the disk as a whole is accelerating down the incline. There are also the three rotational fictitious forces, Coriolis, Centrifugal, and Euler. In this case, I believe that Centrifugal points away from the center of the disk, Euler points up the incline, and Coriolis has both components, although I may be wrong here.
Roughly speaking, you know that some such fictitious forces must exist by the following argument. In the N frame, the resultant force on the point mass has at least a component pointing radially towards the center of the disk and another pointing down the incline. After all, it is rotating around the center of the disk and the whole disk is going down the incline. If you just naively transform these two components to the rotating frame, E, the result would certainly not be zero. But, the point mass is supposed to be at rest in the frame E! So the over-all fictitious force in the E-frame must have a component pointing away from the center of the disk and another pointing up the incline.
If it isn't already obvious, generally speaking, fictitious forces are best avoided when possible. Of course, sometimes you really can't; for example, the Coriolis force is the reason why hurricanes rotate in the counter-clockwise direction in the northern hemisphere and clockwise in the southern hemisphere (as viewed from above).
The answer to your last question is "no", as you guessed. The disk is accelerating down the incline and so the point of contact between the disk and the incline is also accelerating down the incline... at the same rate. However, in this case, the only fictitious force is the linear one. In this frame, the disk does not move linearly, it just rotates and as it does the incline "slides" underneath it faster and faster. Linearly accelerated frames are pretty much as easy to deal with as inertial ones.