Earth rotates about its axis with angular velocity ω. An object weighed by a spring balance gives the same reading at the equator and at a height h above the poles (h << R) By assuming the acceleration due to gravity to be same at the equator and at poles without rotating earth, then the value of h is

1
\(\frac{{{\omega ^2}{R^2}}}{g}\)
2
\(\frac{{{\omega ^2}{R^2}}}{{2g}}\)
3
\(\frac{{2{\omega ^2}{R^2}}}{g}\)
4
\(\frac{{\sqrt {Rg} }}{\omega }\)

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