The Kepler space telescope's findings affect the two planet-related parameters in the equation: fp and ne. From that telescope's findings, it is evident that fp is close to 1. I won't say equals because of binary-star systems like Alpha Centauri, where the only places that planets can be stable is either close to one of the stars or else far from the two of them taken together.
But ne is not adequately addressed by that telescope's findings. The Earth around the Sun would be a borderline detection for it, but it has detected lots of planets only a little larger than the Earth, larger by a factor of 1.5 or 2.
Since it detects transits, the telescope only gets sizes directly. To measure planets' masses, one needs to do a radial-velocity detection with a telescope with a high-resolution spectroscope, or else one has to find Transit Timing Variations (TTV's). Many of these can be modeled as orbit perturbations caused by other planets' gravity, and the effects of their gravity will be enhanced by the planets being in an orbital resonance. The downside is that those effects are only big because they add up over each orbit that each planet does. But Kepler observed several planets long enough to get good TTV data, and that has given us estimates of some planets' masses.
From a planet's mass and radius, one can get its average density, but one has to be careful, since a large-enough planet will be centrally condensed because of its interior pressure. From
Planet Models, I calculate that without compression effects, the Earth would be about 10% larger than it is, and its average density would be around 4.3 g/cm^3 instead of its actual 5.5 g/cm^3.
So far, only a few Earth-size planets have measured masses, and those measurements have large error bars. But for TRAPPIST-1, that is enough to suggest that some such planets have super oceans of water, or even lots of hydrogen and helium. Having lots of H2O or H/He can be a problem for habitability, by making it hard for organisms to live near the planet's visible surface, even if hydrothermal vents can still exist.
So ne is up in the air. Many Earth-mass planets may be water worlds, with huge oceans hundreds of mi/km deep, or else they may have very little water and other volatiles, and thus very thin atmospheres.