A set of interrelated components that form a working unit
Key components of a system
Flows
Inputs
Stores
Components
Matter
Output
Open system
Energy and matter can be transferred into the surrounding environment
Closed system
Energy is transferred into and beyond the system, but matter is only cycled between the stores
Isolated system
No interactions with anything outside of the system boundary
Examples of systems
Drainage basin (open system)
Carbon cycle (closed system)
Dynamic equilibrium
Inputs and outputs in the system are in balance
Positive feedback
The effects of an action get amplified or multiplied by knock-on effects
Negative feedback
Nullifies the change and tries to restore equilibrium
Earth system components
Hydrosphere
Atmosphere
Lithosphere
Biosphere
Hydrosphere
All water, liquid, solid and gas
Atmosphere
Layer of gas
Biosphere
Living things
Lithosphere
Outermost part of the Earth's crust
3% of water is fresh, 70% is frozen, 1% is surface water
50% of fresh water is in lakes, 40% in soil, 10% in other sources
Evaporation
1. Occurs when water changes from liquid to gas
2. Depends on solar radiation, temperature, water supply, dry air
Transpiration
Process by which moisture is lost from plant leaves
Cloud formation
Unequal heating causes hot air to rise and cool, reaching saturation point and condensing
Sublimation
Direct change from solid to gas, bypassing the liquid stage
Deposition
Direct change from gas to solid, bypassing the liquid stage
Winds blow from high to low pressure, curved by Coriolis force
Atmospheric circulation cells
Polar cell
Hadley cell
Ferrel cell
Drainage basin
1. Area of land a river drains
2. Includes soil water, groundwater, stemflow, overland flow, throughflow, percolation
Water balance shows long-term average inputs, stores and outputs in a system
Infiltration capacity
Can be compared to the rate of infiltration
Inputs in the water cycle diagram
Precipitation
Interception
Groundwater
Soil water
Surface storage
Flows in the water cycle diagram
Stemflow
Infiltration
Percolation
Throughflow
Groundwater flow
Outputs in the water cycle diagram
Transpiration
Evaporation
Channel flow
Water balance
The long-term relationship between inputs, outputs and stores in a basin
Calculating the water balance
P = Q + E + ΔS
Positive water balance
Typically wet
Negative water balance
Typically dry
Water balance
Changes seasonally - more surplus in winter, more use in summer
The water balance affects how much water is stored in the drainage basin
Features on a flood hydrograph
Lag time
Peak discharge
Bankfull discharge
Rising limb
Receding limb
Rainfall
Baseflow
Humans impact the water cycle through
Soil drainage
Abstraction
Deforestation
Soil damage from farming practices, deforestation increasing erosion and throughflow, and over-abstraction causing droughts are examples of human impacts on the water cycle
Land use change and urbanisation can increase surface runoff and reduce transpiration, leading to drier air
River Eden basin
Higher than national average rainfall due to relief
Steep slopes impacting lag time and discharge
Impermeable igneous rock in the west, permeable limestone in other areas