To understand the Coriolis Effect mathematically, scientists use an equation:
F = 2 * m * v * Ο * sin(ΞΈ)
In this formula:
- F is the
Coriolis force,
- m is the mass of the object,
- v is the velocity (speed and direction of movement),
- Ο represents the Earth's rotational speed, and
- ΞΈ is the latitude (how far north or south you are from the equator).
This equation helps predict how much an object will curve depending on where it is on Earth and how fast it's moving! π