Open Access

Fig. 13.

image

Dependence of the cycle amplitude on the convection zone diffusivity (ηc) at different peak meridional flow speeds (Vθp). For high peak meridional flow speed (Vθp = 15, 20 m s−1), the cycle amplitude first increases and then decreases with increasing ηc, whereas for low peak meridional flow speed (Vθp = 10, 12.5 m s−1), the cycle amplitude continuously decreases with increasing ηc.

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