Step 1: Conservation of Angular Momentum:
Since there is no external torque acting on the Earth, its angular momentum ($L$) remains constant.
\[ L = I\omega = \text{constant} \]
Step 2: Change in Moment of Inertia ($I$):
Water flows from the poles (distance from axis $r \approx 0$) to the equator (distance from axis $r = R$).
Since mass is moving to a larger distance from the axis of rotation, the moment of inertia $I = \sum mr^2$ increases.
Step 3: Effect on Time Period:
Since $L = I\omega$ is constant and $I$ increases, the angular velocity $\omega$ must decrease.
The duration of the day is $T = \frac{2\pi}{\omega}$.
As $\omega$ decreases, $T$ increases.
Conclusion:
Angular momentum is constant, and the duration of the day increases.