Tributärzuflüsse
Tributärzuflüsse, also known as tributary flows, are streams and rivers that flow into a larger river or a waterbody. These streams are typically smaller than the main river and are often fed by surface runoff or groundwater.
Tributärzuflüsse play an essential role in the hydrological cycle. They contribute to the flow rate of the
There are different types of tributary flows, including perennial streams, which flow year-round, and intermittent streams,
Identifying and characterizing tributary flows is crucial for water resource management and flood risk assessment. Hydrologists
Tributary flows can also be affected by human activities, such as land use changes and channel alterations.