Unit 1, hydrology and fluvial geomorphology Flashcards
Outputs of the drainage basin
Transpiration, evaporation, river channel flow.
Inputs of the drainage basin
Precipitation.
Stores of the drainage basin
Interception, surface storage, soil moisture storage, groundwater storage, channel storage.
Flows of the drainage basin
Overland flow, infiltration, percolation, throughflow, groundwater flow.
Components of hydrographs
Discharge, rising limb, falling limb, peak discharge, lag time.
Discharge definition
Amount of water passing every second.
Rising limb definition.
The rapid increase in resulting from rainfall causing overland flow.
Falling limb definition
When discharge decreases and the river’s level falls.
Peak discharge definition
Time of the highest river channel level.
Lag time definition
The amount of time between the peak amount of rainfall and the peak discharge in the river.
Influences on hydrographs
Shape of the drainage basin, heavy storms, snowfall, vegetation, rock type, deforestation, afforestation, urbanisation, reservoirs, agriculture.
How does climate and temperatures affect a storm hydrograph?
Hot, dry conditions and cold, freezing conditions result in hard ground, reducing infiltration and increasing surface runoff, this leads to a reduced lag time and peak discharge. High temperatures can also increase evapotranspiration, reducing the amount of water reaching the river channel and peak discharge.
Drainage basin characteristics
Size, shape, slope, rock type, soil type, drainage density, rainfall type and rainfall intensity.
Basin size
A large drainage basin will mean that water takes a long time to travel through tributaries or the ground to reach the channel.
Basin Shape
Circular basins mean shorter lag times and higher peak discharges and elongated basins, longer lag times and lower peak discharges.
Slope
A steeply-sided river valley means that gravity assists water in its descent towards the river channel, whereas gently sloping valleys tends to produce longer lag times and lower peak discharges.
Rock type
Permeable rocks such as chalk and limestone infiltrate water so longer lag times and lower peak discharges, and impermeable rocks such as granite and clay allow water to continue to move so this results in shorter time lags and higher peak discharges.