Step 1: Understanding the Concept:
The hydrologic cycle describes the continuous movement of water on, above, and below the surface of the Earth.
Precipitation falling on a watershed is distributed into various pathways: some returns to the atmosphere, some sinks into the ground, and some travels to surface water bodies.
Step 2: Detailed Explanation:
- Runoff is defined as that portion of precipitation that reaches the stream channel by a variety of paths above and below the surface of the earth.
It consists of three main components:
1. Surface Runoff (Overland Flow): Water that travels across the land surface directly into stream channels.
2. Subsurface Runoff (Interflow): Water that infiltrates the upper soil layers and moves laterally through the unsaturated zone to reach the stream.
3. Groundwater Runoff (Baseflow): Water that infiltrates deep into the saturated zone and slowly discharges into the stream channel over a longer period.
Let us review the other options:
- Streamflow is the actual discharge of water flowing within a defined river or stream channel.
It is the physical measurement of water in the channel (\(\text{m}^3/\text{s}\)).
- Infiltration is the process of water entering the soil surface from above.
- Overland flow is only the surface component of runoff before it enters a defined channel.
Therefore, runoff is the broad term for the entire portion of precipitation that reaches the stream through all above and below-ground pathways.
Step 3: Final Answer:
The portion of precipitation reaching the stream channel via various paths above and below the surface is Runoff.