HIGHLIGHTS
- What: Items and_(3) are focal points of this paper and explored within the configuration for rotating Rayleigh-Bénard convection (RRBC) within the tilted f -plane approximation located at an arbitrary colatitude ϑf. The authors demonstrate in this section that away from the equatorial region (i.e. for γ=o(ε-1/2 )), the system of boundary-layer equations valid in the Ekman layer have the classical ODE form for the upright case consisting of a fourth-order linear operator in space albeit now operating in the axial direction. Through linear stability analysis, the authors seek to show . . .

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