“…The velocity downshifted portion of the wave spectrum fills the spectral gap in the Landau plateau providing high energy electrons for the high velocity component of the spectrum to damp on. Various mechanisms have been proposed as sources of the downshift that provides spectral gap closure including: geometric downshift of the wave velocity [21,22,23], wave interactions with turbulence [21,22,17,24,25], diffractional broadening of the wave spectrum [26,27,28,29,30], and spectral broadening as a result of parametric wave interactions [31,17]. As each of these effects modify the wave spectrum differently, if the dominant effect or combination of effects is not properly included in a simulation then its results may differ substantially from the experimental measurements.…”