Coriolis Force Equation:
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The Coriolis effect is an apparent force that acts on objects moving in a rotating reference frame, such as the Earth. It causes moving objects to be deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere.
The calculator uses the Coriolis force equation:
Where:
Explanation: The equation calculates the apparent force experienced by a moving object due to the Earth's rotation, with the effect being strongest at the poles and zero at the equator.
Details: Understanding the Coriolis effect is crucial in meteorology, oceanography, and ballistics. It influences weather patterns, ocean currents, and the trajectory of long-range projectiles.
Tips: Enter angular velocity in radians per second (Earth's is approximately 7.292115 × 10-5 rad/s), latitude in radians (convert from degrees by multiplying by π/180), and velocity in meters per second.
Q1: Why does the Coriolis effect occur?
A: It occurs because different points on a rotating sphere have different linear velocities, causing apparent deflection of moving objects.
Q2: How does latitude affect the Coriolis force?
A: The effect is strongest at the poles (where sin(lat) = ±1) and zero at the equator (where sin(lat) = 0).
Q3: What is the Earth's angular velocity?
A: Approximately 7.292115 × 10-5 radians per second (2π radians per sidereal day).
Q4: Does the Coriolis effect influence small-scale phenomena?
A: No, it's only significant for large-scale or long-duration movements like weather systems or ocean currents.
Q5: How does the Coriolis force affect weather systems?
A: It causes cyclones to rotate counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere.