The movement of water between stores in the hydrological cycle
Groundwater
Water contained within the soil or underlying rocks, derived mainly from percolation of rainwater and meltwater
Stores
Features that receive, hold, and release water (RHR)
Hydrological cycle
The global movement of water between the air, land, and sea
Aquifer
Permeable rock capable of holding and transferring underground water
Evapotranspiration is the combined process in which water moves from the earth’s surface into the atmosphere
Open system
A set of interrelated objects where there are both inputs and outputs
Percolation is the downward movement of water from the soil to the rock beneath
Permeable
Allowing liquids or gases to pass through
Flows
Steady streams of movement from one point to another
Storm hydrographs show the change in river discharge after a storm event
Transfers within water cycle
1. Evaporation
2. Condensation
3. Transpiration
4. Evapotranspiration
5. Precipitation
6. Overland flow
7. Infiltration
8. Percolation
9. Throughflow
10. Groundwater flow
Parts of a drainage basin include Source, Tributary, Confluence, Estuary, and Watershed
Channel network is the collection of all the channels in a given drainage basin
Infiltration is the process in which water on the ground surface enters the soil
Lag time is the delay between peak rainfall and peak discharge
Storm flow is the additional discharge of the river after a storm event
Factors affecting river regimes include Temperature, Climate, and Precipitation
Hydrograph is a graph showing the discharge of a river over a given period of time
Outputs of drainage basins include the river’s discharge and water that evaporates and transpires from the basin and eventually lands in another drainage basin
Drainage basin is an area that is drained by a river and its tributaries; it is an open system
Groundwater flow is the underground transfer of water to rivers, lakes, and seas (water bodies)
Abstraction is the removal of water from rivers, lakes, and from below the water table (R,L,BW)
Reservoirs
An area where water is collected and stored for human use
Closed system
A system that has no inputs or outputs
Meltwater
Water formed by the melting of snow and ice
Interception
The retention (holding) of water by plants and soil which is then evaporated and sent to the atmosphere or absorbed by vegetation
Throughflow is when water moves slowly through the soil between the ground surface and the top of the groundwater store until it reaches a stream/river
Overland flow occurs when precipitation hits the ground, moves due to gravity, and eventually reaches a water body
River Discharge is the quantity of water flowing in a river channel at a particular location and time
Dams are large structures built across a river to hold back a large body of water (reservoir) for human use
Inputs of drainage basins include energy from the sun, precipitation, and water from tributary drainage basins
Base flow is the ‘normal’ discharge in a river
River regime is the seasonal changes of discharge in a river
Climate - High temps
More evaporation → reduce discharge
Vegetation - Trees/plants
Intercept and delay water reaching the ground → reduce overland flow → reduces discharge
Rock type - Permeable rocks
Slows delivery of water to river
Land use - Turmac & concrete in urban areas
Impermeable → speeds up run off and reduces lag time
Deposition - The dropping off of material by river when it doesn’t have the energy to carry them
Vertical erosion - Increases depth of river and is dominant in the upper course of the river