Abstract
We elucidate the role of zonal flows in transient phenomena observed during transition by studying a simple transition model which contains the evolution of zonal flows, mean flows, and the ion pressure gradient. Zonal flows are shown to trigger the transition and cause time-transient behavior through the self-regulation of turbulence before a mean shearing, due to a steep pressure profile, secures a quiescent mode. Surprisingly, this self-regulation lowers the power threshold for the ultimate transition to a quiescent -mode state.
- Received 24 January 2003
DOI:https://doi.org/10.1103/PhysRevLett.90.185006
©2003 American Physical Society