1. Mass (m) of the object: The heavier the object, the stronger the Coriolis force acting on it.

2. Speed (v) of the object: The faster the object is moving, the stronger the Coriolis force.

3. Latitude (φ): The Coriolis force is strongest at the poles (φ = 90°) and weakest at the equator (φ = 0°). It increases proportionally to the sine of the latitude.

In a nutshell:

* Heavier, faster objects at higher latitudes experience the strongest Coriolis force.

It's important to note that the Coriolis force is a fictitious force that arises from the rotation of the Earth. It's not a real force like gravity, but rather an apparent force that acts on objects moving in a rotating frame of reference.