To determine the value of quick flow (Q), we need to use the water balance equation.
- Precipitation (P): The total amount of water falling as rain, snow, etc., in a given area and time.
- Evapotranspiration (ET): The sum of evaporation and plant transpiration from the Earth's land surface to the atmosphere.
- Change in Storage (ΔS): The change in the amount of water stored in the region (e.g., in soil, groundwater, surface water).
- Quick Flow (Q): The component of streamflow that responds rapidly to precipitation events; also known as surface runoff or direct runoff.
The water balance equation states that the total inflow of water into a region must equal the total outflow plus the change in storage. In this case, the equation is: \[ P = ET + Q + \Delta S \]
\( P = 450 \text{ mm/year} \)
\( ET = 200 \text{ mm/year} \)
\( \Delta S = 80 \text{ mm/year} \)
We need to rearrange the water balance equation to solve for Q: \[ Q = P - ET - \Delta S \] Substituting the given values: \[ Q = 450 - 200 - 80 = 170 \text{ mm/year} \]
The value of quick flow (Q) is 170 mm/year.