“…The Boussinesq approximation is justified and generally used for modelling convection in Earth's inner core where density variation between the inner-outer core boundary and the core mantle boundary is small [13,14,38,47]. The density contrast between the bottom (ρ i ) and the top (ρ o ) of the Solar convection zone is five orders of magnitude giving a density scale number of log(ρ i /ρ o ) ≈ 12 [62], and the anelastic approximation is more appropriate and commonly used in global solar convection models, for example, [11,33,63]. However, anelastic and Boussinesq simulations show many similarities [63], with Boussinesq models able to mimic solar periodicity and active longitude phenomena [25,42].…”