Is a deep one-cell meridional circulation essential for the flux transport Solar Dynamo?
Gopal Hazra, Bidya Binay Karak, Arnab Rai Choudhuri

TL;DR
This study investigates whether a shallow return flow in the Sun's meridional circulation can sustain the flux transport dynamo, finding that an equatorward flow at the convection zone's bottom is crucial for solar-like magnetic cycle features.
Contribution
The paper demonstrates that a shallow return flow can still produce solar-like dynamo behavior if an equatorward flow exists at the convection zone's base, challenging the traditional one-cell circulation assumption.
Findings
Equatorward flow at the convection zone's bottom is essential.
Low diffusivity leads to unrealistic cycle periods.
Radially downward pumping improves solar-like behavior.
Abstract
The solar activity cycle is successfully modeled by the flux transport dynamo, in which the meridional circulation of the Sun plays an important role. Most of the kinematic dynamo simulations assume a one-cell structure of the meridional circulation within the convection zone, with the equatorward return flow at its bottom. In view of the recent claims that the return flow occurs at a much shallower depth, we explore whether a meridional circulation with such a shallow return flow can still retain the attractive features of the flux transport dynamo (such as a proper butterfly diagram, the proper phase relation between the toroidal and poloidal fields). We consider additional cells of the meridional circulation below the shallow return flow---both the case of multiple cells radially stacked above one another and the case of more complicated cell patterns. As long as there is an…
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