An apparent, rather than real, force which causes the deflection of moving objects, especially of air streams, through the rotation of the earth on its axis. It shows up, for example, in the movement of an air stream, relative to the rotating earth beneath it. It is equal to -2Ω × V, where Ω is the angular velocity of the earth, and V is the (relative) velocity of the air stream. This apparent force has its greatest deflective effect at the poles, and its least at the equator, this deflection reducing efficiency of an atmospheric cell to transport heat polewards.
The Coriolis parameter is equal to the component of the earth's vorticity about the local vertical and, at latitude φ, is 2Ωsin φ. For a horizontally moving air parcel, the magnitude of the horizontal Coriolis force on the parcel is the product of its velocity and the Coriolis parameter.