Runoff mostly happens in the form of high runoff discharge events that occur in a very short period (called flash floods).
These are related to the steep topography, often little vegetation cover and intense convective rainfall.
The peaks of such flash floods have often a 50 to 100 times larger discharge than the preceding baseflow.

The magnitude of floods in this river has however been decreased due to interventions in the catchment.

At the upper catchment, an exclosure has been established; the dense vegetation largely contributes to enhanced infiltration, less flooding and better baseflow.
Physical conservation structures such as stone bunds and check dams also intercept runoff.
Runoff mostly happens in the form of high runoff discharge events that occur in a very short period (called flash floods). These are related to the steep topography, often little vegetation cover and intense convective rainfall. The peaks of such flash floods have often a 50 to 100 times larger discharge than the preceding baseflow.
The magnitude of floods in this river has however been decreased due to interventions in the catchment. 
At the upper catchment, an exclosure has been established; the dense vegetation largely contributes to enhanced infiltration, less flooding and better baseflow. Physical conservation structures such as stone bunds and check dams also intercept runoff.
Graliwdo