Planar Nonlinear Galloping of Iced Transmission Lines under Forced Self-Excitation Conditions

<div>The curves of excitation amplitude (<i>p</i>) and response amplitude (<i>a</i>). (a) Different wind velocities (<i>σ</i> = 0.5). (b) Different wind velocities and tuning parameters.</div>

Discrete Dynamics in Nature and Society

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Figure 7

Figure 7: Planar Nonlinear Galloping of Iced Transmission Lines under Forced Self-Excitation Conditions 