collected by the surface detector array of the Pierre Auger Observatory over more than 14 yr.
We determine the equatorial dipole component, ${{\boldsymbol{d}}}_{\perp }$ … More precise
measurements of the large-scale anisotropies, filling the gap between the IceCube/IceTop or
KASCADE-Grande measurements and the dipole determined by the Pierre Auger Observatory
above 8 EeV, should provide information about this transition. In fact, although at energies …