Water And Carbon New Flashcards
Inputs
Matter or energy is added to the system
Outputs
Matter or energy leaves the system
Stores
Matter or energy builds up in the system
Flows
Matter or energy moves in the system,
Boundaries
Limits to the system
E.g watershed
Open system
System receives inputs and transfers outputs
Closed systems
Energy inputs equal outputs
Dynamic equilibrium
Inputs dual outputs despite changing conditions
Positive feedback
Chain of events amplifies the impacts the original event
Negative feedbacks
Chain of events that nullifies the impacts of the original event
Leads to dynamic equilibrium
In a local drainage basin, how may water be lost as an output
Evapotranspiration
Runoff
Input of precipitation
Water that falls to the surface of the earth from the atmosphere- rain, snow, hail
What are the 3 types of rainfall
State only
Conventional
Relief
Frontal
Conventional rainfall
Due to heating by the sun
Warm air rises
Condenses in the higher altitudes
Falls as rain
Relief rainfall
Warm air is forced upwards
By a barrier such as mountains
Causes it to condense
Falls as rain
Frontal rainfall
Warm air rises over cool air
Two bodies of different temperatures
Warm air is les dense and lighter
Condenses at higher altitudes and falls as rain
Output- Evapotranspiration
Compromised of evaporation and transpiration
Flows- infiltration
Process of water moving from above the ground into the soil
Flows- percolation
Inputs
Matter or energy is added to the system
Outputs
Matter or energy leaves the system
Stores
When matter or energy builds up
Flows
Matter or energy moves from one store to another
Boundaries
Limits of the system
Open system
Energy and matter CAN enter and leave an open system
Closed system
Matter CANT enter or leave
Energy CAN enter and leave
Equilibrium
Flows and processes continue to happen but there’s no overall changes to the system
Positive feedback
Mechanisms amplify the change in the inputs or outputs
System responds by increasing the effects of the change in
Moves the system even further from it previous state
Negative feedback
Mechanisms counteract the change in the inputs or outputs
System responds by decreasing the effects of the change in Moves
Keeps the system closer to its previous state
Cryosphere
Includes all the parts of the earth where it’s cold enough for water to freeze.
Glacial landscapes
Lithosphere
The outermost part of the earth
Incudes the crust and the upper parts of the mantle
Biosphere
Part of the earths system where living things are found
Includes all the living parts of the earth
Plants, animals, birds, fungi, insects, bacteria etc.
Hydrosphere
Includes all the water on the earth
Can be in a liquid form- lakes and rivers
Solid form- ice
Gas- water vapour
Can also be saline- salty or fresh.
Atmosph
Layer of gas between the earths surface and space, held in place by gravity
Throughflow
Water moves through the soil and into streams or rivers
Speed of flow is dependent on the type of soil.
Clay- slower flow rate
Sandy soils- quickly
Surface run off
Water flows above the ground
Groundwater flow
Water moves through the rocks
Streamflow
Water that moves through established channels- fast
Stem flow
Flow of water that has been intercepted by plants or trees, down a stem, leaf, branch or the other part of a plant
Stores- soil water
Water that is stored in the soil which is utilised by plants
Stores- groundwater
Water that is stored in the pore spaces of rock
Stores- interception
Water intercepted by plants or their branches and leaves before reaching the ground
What’s the water balance
Used ti express the process of water storage and transfer in a drainage basin
How can the water cycle be impacted on a local scale
Deforestation
Storm events
Seasonal changes
Agriculture
Urbanisation
Changes to the water cycle- deforestation
Less interception by trees so surface runoff increases
Soil is no longer held together by roots
So soil water storage decreases
Fewer plants- transpiration decreases
Changes to the water cycle- storm events
Large amounts of rainfall
Saturates the ground
What does the soil water budget show
Shows the annual balance between inputs and outputs in the water cycle and their impact on soil water storage/ availability
What is the soil water budget dependant on
Type
Depth
Permeability of the soils nd bedrock
Seasonal variation of the soil water budget- autumn
Greater input from precipitation than there is an output from Evapotranspiration.
Seasonal variation of the soil water budget- winter
Potential Evapotranspiration from pants reach a minimum due to the colder temperatures
Seasonal variation of the soil water budget- spring
Potential Evapotranspiration increases as temperature get higher and plants start photosynthesising more
Still water surplus
How can the water cycle change over time
Seasonal changes
Storm events
Droughts
El Niño
Human impacts on the water cycle
Farming practices
Land use change
Water abstraction
What is a flood hydrograph is used to represent
Rainfall for the drainage basin of a river and the discharge of the same river on a graph
Flood hydrograph: discharge
Volume of water passing through a cross-sectional point of the river at any one point in time
Measured in cumecs
Flood hydrograph- rising limb
The line on the groan that represents the discharge increasing
Flood hydrograph- falling limb
The line on the graph that represents the discharge deceasing
Flood hydrograph- lag time
The time between peak rainfall and peak discharge
Flood hydrograph- base flow
The level of groundwater flow
Flood hydrograph- storm flow
Comprised of overland flow and throughflow
Flood hydrograph- bankfull discharge
Max capacity of the river.
Flashy hydrograph
Short lag time and high peak discharge
Most likely to occur during a storm event, with favourable drainage basin characteristics
Features of a flashy hydrograph
Short lag time
Steep rising and falling limb
Higher flood risk
Higher peak discharge
Features of a subdued hydrograph
Long lag time
Gradually rising and falling limb
Lower flood risk
Low peak discharge
Combustion
When fossils fuels and organic matter such as trees are burnt
They admit co2 into the atmosphere that was previously locked inside of them.
Decomposition
When living organisms die they are broken down by decomposes which respire
Returning c02 into the atmosphere
Diffusion
Oceans can absorb c02 from the atmosphere which has increased ocean acidity
Weathering and erosion
Rocks are eroded on land or broken down by carbonation weathering.
Burial and compaction
When shelled marine organisms die their shells fall onto the ocean floor and become compacted over time to form limestone.
Carbon sequestration
Transfer of carbon from the atmosphere to other stores and can be both natural and artificial
Causes of the enhanced greenhouse effect
Land use change
Fertilisers
Deforestation
Urbanisation