Gravity Acceleration Formula:
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Local gravity acceleration (g) varies with latitude and altitude due to Earth's shape, rotation, and mass distribution. The standard gravity value of 9.80665 m/s² is an average that changes based on geographic location.
The calculator uses the international gravity formula:
Where:
Explanation: The formula accounts for Earth's ellipsoidal shape (latitude effect) and the decrease in gravity with altitude.
Details: Accurate local gravity values are essential for precision measurements in geophysics, engineering, metrology, and scientific research where gravitational effects are significant.
Tips: Enter latitude in degrees (-90° to 90°, negative for Southern Hemisphere) and altitude in meters above sea level. Values must be within valid ranges.
Q1: Why does gravity vary with latitude?
A: Earth's rotation creates centrifugal force that reduces effective gravity, and the equatorial bulge means you're farther from Earth's center at the equator.
Q2: How much does gravity change with altitude?
A: Gravity decreases by approximately 0.000003086 m/s² per meter of altitude increase.
Q3: What is the range of gravity on Earth's surface?
A: Gravity ranges from about 9.7639 m/s² at Mount Nevado Huascarán (Peru) to 9.8337 m/s² at the Arctic Ocean surface.
Q4: Does local geology affect gravity?
A: Yes, dense rock formations can increase local gravity by 0.0001-0.0005 m/s², while less dense areas show slightly lower values.
Q5: How accurate is this calculation?
A: This provides theoretical values accurate to about ±0.001 m/s² for most locations, but precise measurements require gravimeter instruments.