A drainage basin is defined as an area of land drained by a river and its tributaries, with watersheds separating adjacent basins, and any precipitation falling beyond a watershed will drain into a neighboring basin; the drainage basin hydrological cycle involves inputs like precipitation, storage in surface waters and groundwater, transfer through runoff, groundwater and subsurface flow, and outputs through rivers draining into seas and losses from evapotranspiration. The document describes the components and processes involved in the drainage basin hydrological cycle, including inputs, storage, transfer, and outputs of water within a bounded drainage basin area.

1. Drainage Basin Hydrological Cycle Smy

3. Learning Objectives: To recognise the components of the drainage basin hydrological cycle To draw a systems diagram to represent the DBHC

4. A drainage basin is an area of land (catchments area) drained by a river and its tributaries. Drainage basins are separated from each other by ridges of land called watersheds. Any precipitation falling beyond the watershed will eventually drain into the neighbouring basin. The drainage basin hydrological cycle may be defined as a single river basin bounded by its own watershed and the sea.

8. Drainage Basin Systems Diagram

9. Inputs The main input to the system is precipitation. The type of precipitation (rain or snow, etc), the intensity, the duration and frequency all have an effect on the amount of water in the system. Each subsystem of the drainage basin system will also have inputs and ouputs, and the output from one stage of the diagram will form the input for another.

10. Storage Water is stored in a drainage basin on the surface in lakes and channels or underground in the groundwater store. Water reaches the groundwater store via the processes of infiltration and percolation. During these processes, some water will be stored in the soil and rock. The amount of water stored will vary depending on the porosity of the soil and on the permeability of the rock. Water can also be temporarily stored via interception. This refers to the storage of water on leaf and plant stems. Dense foliage may result in little water reaching the ground, since it often evaporates from the leaves.

11. Transfer The sum of all the water flowing over the drainage basin’s surface is called runoff. It is made up of streamflow, which is flow through permanent river channels and overland flow or surface runoff. Overland flow transfers water through the basin either as sheetwash, across the surface, or in tiny channels called rills. Beneath the surface, water is transferred via throughflow, which is the movement of water through the lower soil towards rivers, and groundwater flow. Groundwater flow is typically very slow. Water that has been intercepted by foliage may also be transferred, either directly as throughfall, or by running down branches and stems via stemflow.

12. Outputs The final release of the water in a drainage basin is known as its output. Typically, rivers flowing into the sea will be the main output of a drainage basin. Some water will also be lost via evapotranspiration. This process refers to direct evaporation, and also to the extend that moisture lost from leaves will result in plants withdrawing water from the soil via their roots.

13. Complete questions 1a,b and c on page 90 of GAIA