FTP, identify this fictitious force exerted on a fast-moving body moving in a non-inertial reference frame.
The magnitude of this effect is inversely proportional to the parameter known as the Rossby number, the ratio of the inertial motion to rotational motion. For cyclostrophic flow it as defined as being equal to zero. The Navier-Stokes equations can be modified to account for it by adding a parameter f which is proportional to the angular velocity and the latitude. It can be seen directly in the uneven erosion of railroad tracks and river beds, and in the spiraling of air from high pressure zones to low pressure zones. FTP, identify this fictitious force exerted on a fast-moving body moving in a non-inertial reference frame.
The magnitude of this effect is inversely proportional to the parameter known as the Rossby number, the ratio of the inertial motion to rotational motion.
Coriolis effect