Coriolis Acceleration Formula:
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The Horizontal Component of Coriolis Acceleration is defined as the acceleration due to the rotation of the earth, experienced by particles (water parcels, for example) moving along the earth's surface. It's a crucial factor in geophysical fluid dynamics and atmospheric sciences.
The calculator uses the Coriolis acceleration formula:
Where:
Explanation: The formula calculates the apparent acceleration experienced by moving objects due to Earth's rotation, which depends on latitude and the object's velocity.
Details: Coriolis acceleration is essential for understanding large-scale atmospheric and oceanic circulation patterns, weather systems, and the behavior of projectiles and aircraft over long distances.
Tips: Enter angular speed of Earth in rad/s (default is approximately 7.2921159×10⁻⁵ rad/s), latitude in degrees (-90 to 90), and current velocity in m/s. All values must be valid.
Q1: Why does Coriolis acceleration depend on latitude?
A: The Coriolis effect is strongest at the poles and zero at the equator because it depends on the component of Earth's rotation perpendicular to the surface.
Q2: What is the typical value of Earth's angular speed?
A: Earth's angular speed is approximately 7.2921159×10⁻⁵ radians per second, which corresponds to one full rotation every 24 hours.
Q3: How does Coriolis acceleration affect ocean currents?
A: Coriolis acceleration causes moving water to deflect to the right in the Northern Hemisphere and to the left in the Southern Hemisphere, influencing major ocean current patterns.
Q4: Is Coriolis acceleration significant for small-scale motions?
A: For small-scale motions over short distances and time periods, Coriolis effects are usually negligible compared to other forces.
Q5: How does Coriolis acceleration affect weather systems?
A: Coriolis acceleration is responsible for the rotation of large-scale weather systems like hurricanes and the direction of prevailing winds.