River discharge is defined as the volume of water passing a measuring point or gauging station in a river in a given time. It is measured in cubic metres per second (cumecs). The overall discharge from the drainage basin depends on the relationship between preciptiation and storage factors and can be summarised as follows:<\/p>\n
Drainage basin discharg= precipitation – evapo-transpiration + or – changes in storage<\/p>\n
Discharge can be illustrated using hydrographs. These can show annual patterns of flow ( the river regime) in response to climate. Short-term variations in discharge are shown using a flood of storm hyrdograph.
\nThe storm hydrograph
\nPicture
\nThe storm hydrograph (shown to the left) shows variations in a river’s discharge over a short period of time, usually during a rainstorm. The starting and finishing level show the base flow of the river. As storm water enters the drainage basin the discharge rises, shown by the rising limb, to reach the peak discharge, which indicates the highest flow in the channel. The receding limb shows the fall in the discharge back to the base level. The time delay between maximum rainfall amount and peak discharge is the lag time.
\nFactors affecting a river’s discharge
\nRock and soil type
\n\u00b7 Permeable rocks ad soils (such as sandy soils) absorb water easily, so surface run-off is rare
\n\u00b7 Impermeable rock and soils (such as clay soils) are more closely packed. Rainwater can\u2019t infiltrate, so water reaches the river more quickly
\n\u00b7 Pervious rocks (like limestone) allow water to pass through joints, and porous rocks (like chalk) have spaces between the rock particles
\nLand use
\n\u00b7 In urban areas, surfaces like roads are impermeable \u2013 water can\u2019t soak into the ground. Instead, it runs into drains, gathers speed and joins rainwater from
\nother drains \u2013 eventually spilling into the river
\n\u00b7 In rural areas, ploughing up and down (instead of across) hillsides creates channels which allow rainwater to reach rivers faster increasing discharge
\n\u00b7 Deforestation means less interception, so rain reaches the ground faster. The ground is likely to become saturated and surface run-off will increase
\nRainfall
\n \u00b7 The amount and type of rainfall will affect a river\u2019s discharge
\n \u00b7 Antecedent rainfall is rain that has already happened. It can mean that the ground has become saturated. Further rain will then flow as surface run-off towards the river
\n\u00b7 Heavy continual rain, or melting snow, means more water flowing into the river
\nRelief
\n\u00b7 Steep slopes mean that rainwater is likely to run straight over the surface before it can infiltrate. On more gentle slopes infiltration is more likely.
\nWeather conditions
\n\u00b7 Hot dry weather can bake the soil, so that when it rains the water can\u2019t soak in. Instead, it will run off the surface, straight into the river.
\n \u00b7 High temperatures increase evaporation rates from water surfaces, and transpiration from plants \u2013 reducing discharge
\n\u00b7 Long periods of extreme cold weather can lead to frozen ground, so that water can\u2019t soak in<\/p>\n","protected":false},"excerpt":{"rendered":"