Coriolis Acceleration Formula:
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Coriolis acceleration is an inertial acceleration that acts on objects moving within a rotating reference frame. It is perpendicular to both the angular velocity vector and the velocity vector of the moving object.
The calculator uses the Coriolis acceleration formula:
Where:
Explanation: The negative sign indicates that the Coriolis force acts in the opposite direction to the cross product of angular velocity and linear velocity vectors.
Details: Coriolis acceleration is crucial in meteorology (weather patterns), oceanography (ocean currents), ballistics (long-range projectiles), and rotating machinery dynamics.
Tips: Enter angular velocity in rad/s, velocity in m/s, and the angle between vectors in degrees (0-180°). All values must be positive and valid.
Q1: What is the physical significance of Coriolis acceleration?
A: It explains the deflection of moving objects on rotating bodies like Earth, causing winds to curve rather than move in straight lines.
Q2: Why is there a negative sign in the formula?
A: The negative sign indicates that the Coriolis force acts in the direction opposite to the cross product result, maintaining conservation of angular momentum.
Q3: Where is Coriolis acceleration most noticeable?
A: Most significant at large scales (weather systems, ocean currents) and high velocities. Negligible for small-scale, slow-moving objects.
Q4: How does Coriolis effect vary with latitude?
A: Maximum at poles, zero at equator. The effective angular velocity component varies as Ω·sin(latitude).
Q5: Can Coriolis acceleration be felt directly?
A: No, it's a fictitious force apparent only in rotating reference frames. We observe its effects rather than feel the acceleration directly.