Coriolis Acceleration Formula:
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Coriolis acceleration is an apparent acceleration that acts on objects moving within a rotating reference frame. It is perpendicular to both the velocity vector of the moving object and the rotation axis of the reference frame.
The calculator uses the Coriolis acceleration formula:
Where:
Explanation: The formula calculates the magnitude of the Coriolis acceleration experienced by an object moving in a rotating reference frame, with the sine term accounting for the latitude dependence.
Details: Coriolis acceleration is crucial in meteorology for understanding wind patterns, in oceanography for ocean currents, in ballistics for projectile motion, and in various engineering applications involving rotating systems.
Tips: Enter angular velocity in rad/s, velocity in m/s, and latitude angle in degrees (-90° to +90°). All values must be valid (angular velocity > 0, velocity > 0, latitude between -90 and 90).
Q1: What is the physical significance of Coriolis acceleration?
A: It represents the apparent deflection of moving objects when viewed from a rotating reference frame, such as the Earth's rotation causing moving air masses to curve.
Q2: Why does latitude affect Coriolis acceleration?
A: The effective component of the Earth's rotation varies with latitude, being maximum at the poles (sin 90° = 1) and zero at the equator (sin 0° = 0).
Q3: What are typical values for Earth's angular velocity?
A: Earth's angular velocity is approximately 7.292 × 10⁻⁵ rad/s, which corresponds to one rotation every 24 hours.
Q4: How does Coriolis acceleration affect weather patterns?
A: It causes moving air masses to deflect to the right in the Northern Hemisphere and to the left in the Southern Hemisphere, influencing wind patterns and storm rotation.
Q5: Is Coriolis acceleration significant for everyday objects?
A: For most everyday motions, Coriolis acceleration is negligible, but it becomes significant for large-scale motions like atmospheric systems, ocean currents, and long-range projectiles.