If we represent earth’s magnetic field at the equator, by B, the dipole moment of earth (radius = R)’s equivalent magnet is given by
(1) \(\frac{4\pi R^3 B}{μ_0}\)
(2) \(\frac{4\pi R^2 B}{μ_0}\)
(3) \(\frac{2\pi RB^2}{μ_0}\)
(4) \(\frac{2\pi RB}{μ_0}\)