To understand what a falling limb of a synthetic unit hydrograph is, we need to define the components of a hydrograph and how they relate to streamflow.
- Hydrograph: A graph showing the rate of flow (discharge) versus time past a specific point in a river, stream, or channel.
- Unit Hydrograph: A hydrograph representing the direct runoff from a watershed due to one unit (e.g., 1 inch or 1 cm) of excess rainfall occurring uniformly over the watershed at a uniform rate during a specified period of time.
- Synthetic Unit Hydrograph: A unit hydrograph derived from empirical equations rather than observed data. This is used when observed data is not available.
- Rising Limb (Ascending Limb): The part of the hydrograph where the discharge is increasing.
- Peak Discharge: The maximum discharge on the hydrograph.
- Falling Limb (Recession Limb or Descending Limb): The part of the hydrograph where the discharge is decreasing after the peak.
The falling limb represents the period after the peak discharge when the streamflow is receding as the contribution from direct runoff diminishes.
- The falling limb is the part where discharge decreases.
- The peak discharge is a single point, not the falling limb.
- The rising limb is where discharge increases.
- The total volume of water is represented by the area under the entire hydrograph, not just the falling limb.
A falling limb of a synthetic unit hydrograph is A part of hydrograph where discharge decreases.