The total energy that a river possesses varies from one stage to another because of changes in the river's height, gradient and speed. In the upper course where the gradient is steep and river is high above sea level, the river has a high gravitational potential energy. In the middle course, the potential gravitational energy is converted to kinetic energy and the gradient begins to level out resulting in the river's velocity increasing.
By the time the river reaches its lower stage, it has no gravitational potential energy but lots of kinetic energy resulting in a high velocity.