Streamflow

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Streamflow, or channel runoff, is the flow of water in streams, rivers, and other channels, and is a major element of the water cycle. It is one component of the runoff of water from the land to waterbodies, the other component being surface runoff. Water flowing in channels comes from surface runoff from adjacent hillslopes, from groundwater flow out of the ground, and from water discharged from pipes. The discharge of water flowing in a channel is measured using stream gauges or can be estimated by the Manning equation. The record of flow over time is called a hydrograph. Flooding occurs when the volume of water exceeds the capacity of the channel.

1 Role in the water cycle
2 Measurement
3 Relationship to the environment
4 Relationship to society
5 See also
6 Reference

[edit] Role in the water cycle

Streamflow is the main mechanism by which water moves from the land to the oceans.

[edit] Measurement

The are a variety of ways to measure the discharge of streamflow. For small streams — a few metres wide or smaller — weirs may be installed.

[edit] Relationship to the environment

Runoff of water in channels is responsible for transport of sediment, nutrients, and pollution downstream.

[edit] Relationship to society

Streamflow confers on society both benefits and hazards. Runoff downstream is a means to collect water for storage in dams for power generation of water abstraction. The flow of water assists transport downstream. When the flow of water exceeds the capacity of the channel, flooding occurs.