It is a proven fact that the most gravitational acceleration of the earth exist on the earth's surface.
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Perfect value of acceleration of 🌎 |
As the gravitational acceleration decreases as we go up from the earth, its value will be zero at one time and the gravitational acceleration will decrease as we go down the earth and the value of the Earth's center will be zero. But the biggest problem is to determine the boundaries of the earth because the earth is not spherical but it is rotating and ecliptical and the atmosphere is located within the boundaries of the earth. Whatever it is, we hold the earth's sea level to the earth's borders for convenience. Earth's gravitational acceleration in the polar region is 983.218 cm/s². The gravitational acceleration of the Earth at a latitude of 45° is 980.665 cm/s². And the Earth's gravitational acceleration at the equator is 978.033z cm per second square. In India the datum adapted for the Great Trigonometrical Survey (GTS) is the mean sea level at Karachi it's latitude of 45°.
The difference between the gravitational acceleration of the Earth's polar and equatorial regions is about ( 983.218 - 978.033 ) = 5.185 cm/sec²
Other hand, we know that polar radius of the earth is 6356.7523 km and equatorial radius of the earth is 6378.1370 km. The difference between the two is about 21.3847 km.
Average radius of the earth is about 6371.009 km
Considering all this information, it is easy to conclude that this shape is due to the diurnal motion of the earth. Due to the diurnal motion of the Earth, the gravitational acceleration of the Earth decreases by about 3.4 cm per second square. Here, ω².R.cos²ф = (2л/T)².(6.357×10⁸).(cos²0°) = [ 2л/ (86164.1)]². (6.378137 × 10⁸ ).1² = 3.392 cm/s² Now, taking R =6378.137 km. = 6.378137 × 10⁸. cm, T= 23h 56m 4.1s = 86164.1 seconds . Thus, due to the diurnal motion of the Earth, the highest gravitational acceleration may decrease by 3.392 cm/sec². Note that this calculation only shows the difference between the gravitational acceleration of the polar region and the equatorial region and does not specify the value of the actual gravitational acceleration.
On the other hand we know that g = G.(M+m)/R² = G.M/R² ( where m neglected )
= G.4/3.лR³.р/R² = G.4/3.л.р. R
Or, g = k.R ------- ( 1 )
here, k is Constant. Because G, 4/3, л and р are Constants. So we get from the equation
g ∝ R
Thus the gravitational acceleration of the earth (g) is directly proportional to the radius of the earth (R). The avarage radius of the earth is about 10.70 km greater than the radius of the polar region and the radius of the equatorial region is about 10.70 km greater than the average radius of the earth. The value of the earth's gravitational acceleration in the polar region is correct because there is no effects on the diurnal motion of the earth. On the other hand, the value of the gravitational acceleration of the earth's equatorial region is not entirely accurate because it is here that the effects of the earth's diurnal motion are greatest.
Now let's see what is the equatorial acceleration of the earth :
So the gravitational acceleration at the polar regions is 983.218 cm/s² Earth's average gravitational acceleration
FAQ
What is the average gravitational acceleration of the earth?
Gravitational acceleration of the earth can be basically divided into two parts namely apparent gravitational acceleration and real gravitational acceleration. Apparent gravitational acceleration in the polar region is 983.218 cm/s², earth's gravitational acceleration at the equator is 978.033 cm/s² and the avarage earth's gravitational acceleration at a latitude of 45° is 980.665 cm/s² but Earth's actual gravitational acceleration is about 983 cm/s²
How much does the value of gravitational acceleration decrease due to the diurnal motion of the earth?
Due to the diurnal motion of the Earth, the highest gravitational acceleration may decrease by 3.392 cm/sec².
Does the Earth's oval shape cause the acceleration of gravity to be less or more?
Gravitational acceleration is only slightly affected by the Earth's oval shape
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