Abstract
Tertiary modes in electrostatic drift-wave turbulence are localized near extrema of the zonal velocity with respect to the radial coordinate . We argue that these modes can be described as quantum harmonic oscillators with complex frequencies, so their spectrum can be readily calculated. The corresponding growth rate is derived within the modified Hasegawa-Wakatani model. We show that equals the primary-instability growth rate plus a term that depends on the local ; hence, the instability threshold is shifted compared to that in homogeneous turbulence. This provides a generic explanation of the well-known yet elusive Dimits shift, which we find explicitly in the Terry-Horton limit. Linearly unstable tertiary modes either saturate due to the evolution of the zonal density or generate radially propagating structures when the shear is sufficiently weakened by viscosity. The Dimits regime ends when such structures are generated continuously.
- Received 13 October 2019
- Revised 11 December 2019
- Accepted 14 January 2020
DOI:https://doi.org/10.1103/PhysRevLett.124.055002
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