Factors Influencing Energy of River

Speed of a River

Speed of a River

Gradient of Channel

Gradient of Channel

Rivers flow downhill from a high attitude due to gravity.

The speed of a river depends on the steepness (also known as gradient) of the channel.

Steep gradient, the river will flow quickly.Gentle gradient, the river will flow slowly

Roughness of Channel

Obstacles (rocks,boulders,etc.) cause friction between the water and the channel, it will slow down river flow and speed.Therefore, smooth channel have higher speed than rough channel.

Wetted Perimeter

Wetted Perimeter

Shapes and sizes of a river channel affects the length and breadth of the channel in contact with the water.

Large wetted perimeter will cause a lot of friction, the speed of river will be low. Small wetted perimeter have less friction, the speed of the river will be high.

Shallow River Water Speed Meter

Volume of Water in a River

Volume of Water in a River

Size of Drainage Basin

Size of Drainage Basin

Bigger drainage area have greater amount of water in a river. It is because there is more surface area for rainfall to fall on, flows over the land as surface runoff or steeps into the ground before reaching the river. Smaller drainage area do not 'collect' as much rain water.

Presence of Vegetation

Presence of Vegetation

Abudant vegetation decreases the amount of surface runoff, thus reducing the amount of water in a river. Sparse vegetation leads to high surface runoff, thus increasing the amount of water in a river.

Permeability of Rocks

Permeability of Rocks

High permeability increases infiltration and decreases surface runoff. Thus, volume of water in the river is low. Low permeability decreases infiltration and increases surface runoff. Thus, volume of water in a river is high.

Climate

Climate

The climate of the area a river flows can affect the volume of water in its channel.

In areas with distinct wet and dry seasons, the amount of water in the channel fluctuates according to the amount of rainfall received during each season. In other areas which are generally dry, the volume of water remains low throughout the year. Rivers found in hot and wet equatorial areas have a high volume of water in their channels.

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