The shape of the Earth is not really a perfect sphere as usually thought
It's like an elliphoid with the two flat regions on the North and and South poles and bulging surface on the equator. So the radius from the Earth's centre to the equator is greater than its radius from its centre to either of the two poles which means that it is closer to the Earth's centre of mass on the two poles than on the equator, and the gravitational pulling force of the Earth on a particke is
F= G (Mm)/r^2 . Where r is the distance between the Earth's centre of mass and the particle , M is the Earth's mass, m is the particle's mass . G is gravitational constant. When the particle is realeased, it will fall toward the Earth's surface with an acceleration called gravitational acceleration, as a result of the gravitational force of the Earth pulling on the particle , F = m*a(g)
F=G(Mm)/r^2 and F =ma(g) ----> ma(g)= GM*m/r^2 or a(g)= GM/r^2
When you substitute the Earth's radius from its centre to the equator in the formula to compute the gravitational acceleration of the particle
a(g) = GM/r^2
where G and M are constant and the Earth's radius from its centre to either the two poles and tge Earth's radius from its centre to the equator,
You can see that the gravitational acceleration at two poles are greater due to the fact that radius from the Earth's centre to the two pole is smaller than the radius from the Earth's centre to the equator
Now consider the Earth's rotational motion around its axis
When it rotates any object on its surface also rotates about its axis , and there are two forces acting on objects. One is the reaction or normal force from the Earth's surface along the radial axis from its centre of mass outward to objects on its surface, and the other force is gravitaional force directed inward toward its centre of mass
So the net force is :
Fnet = Fn - ma (g) = ma(r)
Where Fn is normal force, ma(g) is the gravitational force,
a(r) is centripetal acceleration which also points toward the Earth's centre of mass along the radial axis "r"
Fn = mg -----> Fnet = mg -ma(g)= ma(r)
Radial acceleration a(r) can also be expressed as:
a(r) = w^2R . Where w is angular velocity of the circular motion,
R is the radius of he circle or circular path of objects on the Earth's surface
So mg -ma(g) = ma(r) can be simplified as :
g - a(g) = a(r) ----> g - a(g) = -w^2R
g = a(g) -w^2R
Where g is free fall acceleration, angular velocity w and the radius R are constant for the same object
Since earlier, a(g) has been prove to be greater at the two poles
Free fall acceleration "g" is also greater at the two poles