The components parallel to the ground of the Coriolis force and the centrifugal force, at mid-latitudes (40°N), are respectively 2ωvsenφ≅4.67×10^(-4) ms^(-2), 1/2ω^ 2Rsen( 2φ) ≅1.62×10^(-2) ms^(-2). Therefore the ground-parallel component of the centrifugal force is much greater than the corresponding component of the Coriolis force. Why does only the effect of the Coriolis force appear in meteorology books for educational use?