First, lets define some terms. Total resistance is made up of skin friction (i.e. tangent to the skin) and residual resistance. Residual resistance is comprised of pressure distribution over the skin (i.e. a force normal to the skin) and air resistance (which again is divided into skin friction and pressure) but we will ignore air resistance for now. One must always remember that the wave/wake train is nothing more than the physical manifestation of the pressure disturbance in the fluid. Even submarines and SWATH demi-hulls make surface waves.
Because the two major components of drag are perpendicular to each other, hull shape is the single largest player between the two. If I had a very thin, smooth, wide plank and towed it to measure it's drag, I would be measuring almost all skin friction and no pressure drag because the pressure drag not only is perpendicular to the direction of travel, it is null because the force on the port side is equal to the force on the starboard side. This is how the constants for skin friction were developed by Froude and others 150 years ago. Now if I had a parachute sea anchor or a thin disk and towed it, I would be measuring almost all pressure drag as the skin friction is now null because it is all offsetting as the flow is radial out from the center.
Of course there are other considerations that vary the relationship between the two. These are some times presented as separate issues but are actually corrections. Such things as surface roughness, kinematic viscosity, water temperature/density, and pressure gradients effect skin friction, and water depth, wave orbitals and fluid motions, hull trim and list, and again water temperature/density for pressure drag. This is why for most drag calculations the assumptions are "isodense, inviscid, and irrotational" for the fluid. The difference in drag between these three assumptions and real world is normally ~5-10% at "normal" speeds but can be as high as 50-200+% at the extremes (slow or fast) depending on what exactly you are trying to measure.