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Neglect the centrifugal acceleration, which is of order ${\omega }^2$, and use the local flat-surface approximation. To zeroth order in $\omega$, the height above $P$ and flight time areInserting this vertical velocity into the Coriolis acceleration gives the eastward componentWith $x(0)=\dot{x}(0)=0$, two integrations yieldto first order. Horizontal velocity is already of order $\omega$, so its effect on vertical acceleration is of order ${\omega }^2$. Thus the flight time remains $T_0$ at this order. The Coriolis deflection of a vertical projectile at landing isThe displacement is westward, and its magnitude is $4\omega v^3\sin \theta /(3g^2)$. The horizontal speed remains westward during the flight: $\dot{x}=-2\omega \sin \theta z_0(t)$. This explains why the eastward acceleration on descent does not cancel the earlier displacement.