“…The general trend is that the Coriolis force modifies convection such as to establish a large scale differential rotation Ω(r, θ) (Brun & Rempel (2009)). Depending on the influence of the Coriolis force, usually mesured by the turbulent Rossby number Ro = ω conv /2Ω 0 ∼ v conv /2Ω 0 d, or a variant, with ω conv , v conv characteristic vorticity and velocity in the convection zone and d the convection zone depth, the resulting differential rotation can be anti-solar (high Ro > 1, with fast poles-slow equator), solar-like (0.2 < Ro < 0.9, with fast equator, slow poles and some constancy at mid latitude of the isocontours of Ω) or Jupiter-like (Ro < 0.1, with cylindrical profile with alternance of prograde and retrograde jets) Matt et al (2011). On Figure 3 we represent these different profiles in models for various masses (0.5, 0.7 and 1.1 Msol) that also include the coupling to a stably stratified radiative interior, thus possessing a tachocline Matt & Brun (2013).…”