“…Unless otherwise stated, we will take the following normalized parameters from the cyclone DIII-D base case as in the gyrokinetic simulations [56,57], but artificially exchange the magnitudes of electron density gradient and electron temperature gradient as in [35]. The mixing ratio of D-T ions is 1:1, ε 0 = 0.1, q = 1.4, ŝ = 0.8, R/L ne = 6.9, R/L Te = 2.2, Leα = 2, LeHe = 1, and both the temperature gradient of D-T ions and helium ash are artificially set as R/L T j = 0.1 ( j = D, T, He) to avoid ITG instability [29,35,58]. Similar artificial treatment by setting R/L T j = 0 has also been used in [51,59,60], and it has been shown that the wavenumber spectrum of the linear growth rate of both trapped electron mode (TEM) instability [61] and CTEM driven zonal flow (ZF) [51] would not been qualitatively changed by slightly increasing R/L T j .…”