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Why is water important
Oceans is 71% of earths surface
Oceans moderate temperature by absorbing heat, storing and releasing it
Clouds reflect 1/5 of incoming solar radiation
Water vapour absorbs long wave radiation
What is water used for?
65-95% of water in all living organisms
Growth, Reproduction, Metabolic processes
Photosynthesis, Respiration, Transpiration
Plants need it for rigidity and xylem vessels to transport
Its a medium for all chemical reactions
Panting, evaporation, sweating cools organisms
Generates electricity, crops, sewage, agriculture
Drinking water
Why is carbon important?
Common chemical element
Stored in carbonate rocks
Proteins, carbs, nucleic acids basic building blocks
Fossil fuels, coal, oil and gas
Oil used in manufacture of plastics/paint
Water cycle
Closed system globally
Open system at smaller scale
Stores of water
Ocean 97%
Ice 2%
aquifers 0.7%
Atmosphere 0.001%
Land
Transfers of water
Evaporation
Transpiration
Precipitation
Inputs of water to atmosphere
Vapour evaporated from ocean, soil, lakes and rivers
Vapour transpired through leaves
Outputs of water from atmosphere
Precipitation
Condensation(fog)
Ablation(melting and sublimation)
Run-off
Meltwater drains from land into rivers/oceans
Percolate
Water into rocks or aquifers
Transfers of carbon
Decomposition
Respiration
Photosynthesis
Oxidation
Weathering
Volcanic activity
Combustion
Stores of carbon
Biomass (Biosphere)
Soil (pedosphere)
Rocks
Sea floor
Ocean (hydrosphere)
Atmosphere
Slow carbon cycle
Rocks, sediment, fossil fuels locked away for millions years
CO2 diffuses from atmosphere into oceans where marine organisms make their shells and skeletons
They fix dissolved carbon
On death organisms sink and over millions years exert heat and pressure and convert into rock
Takes around 150 mil years
Some subduct into tectonic plates and come out in volcanic eruptions
Other attacked by chemical weathering
Fast carbon cycle
circulates rapidly between atmosphere, oceans, organisms and soil
10-1000x faster than slow carbon cycle
Plants and phytoplankton are key
Absorb CO2 through photosynthesis with water to make carbohydrates
Respiration releases CO2
Decomposition of dead organic material by microbial activity releases CO2
Atmospheric CO2 dissolves ocean surface water and ocean ventilates CO2 back to atmosphere
Carbon is stored in ocean by natural sequestration for about 350 yrs
Precipitation (of water)
Water/ice that falls from clouds
Rain, snow, hail, sleet, drizzle
Forms when vapour cools to due point and condenses into droplets forming clouds
Droplets aggregate and leave clouds
Rain flows quickly into rivers
Snow settles at high altitudes
What is intensity of rainfall?
The amount of precipitation falling in a given time
Transpiration
Diffusion of water vapour to atmosphere from leaf pores (stomata)
Influenced by temperature and wind
Influenced by water availability in plants
Condensation
When vapour turns to liquid water
Happens when air cooled to due point
At critical temp air is saturated with vapour and becomes condensation
Condensation near the ground produces dew and fog
Cumuliform Clouds
Flat base
Form when air heated through contact with earths surface
Causes convection and cooling
Stratiform Clouds
Have layers
Form when air moves horizontal across a cooler surface (advection)
Cirrus Clouds
Form at high altitude
Have tiny ice crystals but don’t form precipitate
Environmental lapse rate
Vertical temperature profile of lower atmosphere at a given time
Dry adiabatic lapse rate
The rate at which a parcel of dry air cools
Saturated adiabatic lapse rate
Rate at which a saturates parcel of air cools as it rises
Why does water vapour cool to due point?
Air is warmed by contact with ground/sea and rises freely through atmosphere
As air rises pressure falls and it cools by expansion (convection)
Air masses move horizontally across cooler surface (advection)
Lapse rates
Vertical distribution of temp in lower atmosphere
Temp changes that occur within an air particle as it rises
How does a cloud form?
Ground heated by sun and air in contact with surface heats to 18 degrees
Air warmer than surroundings so less dense
Atmospheric instability so a convection current forms
Temp reaches due point (8 degrees) and condensation occurs forming clouds
Air rises as long as internal cloud temp is higher than atmosphere
When equilibrium between cloud and atmosphere reached moisture evaporates or precipitates
Throughfall
Rainwater that’s intercepted
Evaporation
Liquid water to vapour
This is the main way water enters atmosphere
Heat needed to break bonds of water
Energy from heat is absorbed as latent heat and released in condensation
Interception
Vegetation intercepts precipitations storing it on branches, leaves and stems
Eventually moisture evaporates and falls to ground
Stemflow
Rainwater flows to the ground along branches
Infiltration
Water flows by gravity into soil and lateral movement to stream or river
Overland flow
Water flows across ground surface as a sheet or trickles to stream or river
Tree species
Conifers have greater interception loss as they have leaves all year round
Vegetation type
Interception is greater from grass than agricultural crops
Wind speed
Evaporation increases with wind speed
Ablation
Loss of ice from snow, glaciers due to sublimation
sublimation
Change of ice to water vapour without becoming a liquid
Precipitation (of carbon)
Atmospheric CO2 dissolves in rainwater to form weak carbonic acid
Rainfall acidity increases due to anthropogenic emissions
Photosynthesis
6CO2 + 6H20 - C6H12O6 +6O2
Plants and phytoplankton carry this out
Use suns energy green plants with chlorophyll convert light energy to chemical energy
Plants use glucose to grow and release CO2 in respiration
Weathering
Breakdown of rocks by chemical, biological and physical processes
Most weathering involves rainwater which has dissolved CO2
Carbonation
calcium carbonate + carbonic acid - calcium bicarbonate
Releases carbon from limestone, rivers, oceans
Respiration
C6H12O6 + 6O2 - 6CO2 +6 H20 + energy
Most organisms respire
Decomposition
Bacteria/fungi break down dead organic matter releasing CO2
This happens fastest in warm, humid environments
Combustion
Organic material reacts or burns in the presence of oxygen
Release CO2
Natural fuel for ecosystems
Wildfire is essential for some ecosystems
Winter slows decomposition
Fire then ensures carbon and nutrients are freed up
Physical Pump
Mixing of surface and deep ocean waters by vertical currents
CO2 enters ocean by diffusion from atmosphere
Downwelling
Water and CO2 are transported by surface currents towards the poles and cool and sink due to density
Carries carbon to ocean depths where it remains for centuries
Upwelling
Deep ocean currents transport carbon to areas of upwelling
It is then diffused back into the atmosphere
Biological pump
Involves marine organisms transferring carbon
Phytoplankton float near surface and photosynthesise
Carbon in phytoplankton accumulates in sediments and is released into ocean CO2
Marine organisms extract carbonate and calcium to manufacture skeletons and shells
most ends up in ocean sediments and is lithified to form chalk/limestone
Vegetation
Trees are huge stores of carbon and are essential to both water and carbon stores
Most carbon rich material is extracted from atmosphere through photosynthesis
Dynamic equilibrium
When natural systems are unaffected by human activity and regulate their own equilibrium
Urbanisation
Land use from rural to urban
Soil/vegetation replaced by impermeable concrete and tarmac
gutters, sewers and roofs remove surface water
Causes more run off and water level rise
Floodplains naturally store water
Urban development reduces water store
Farming
Forests are cleared for farms
Reduces carbon store in vegetation, soil and biomass
Soil carbon in pedosphere reduced by ploughing as exposure to oxidation
Lack of biodiversity reduces carbon store
Crop irrigation diverts water from rivers and groundwater towards land
Interception reduced
Surface run off increases where machinery compacts soil
How does forestry management affect water cycle?
Higher in interception in plantations than forests
Conifers are evergreen so high interception
Increased evaporation as more water stored on leaves
Reduced run off as evaporation, interception and absorption by roots is all high
Transpiration increases
Harvesting timber increase run off, evapotranspiration and discharge
How does forestry management affect the carbon cycle?
Mature forests store tonnes of carbon (10x higher than grassland)
Soil has even larger amounts carbon
Forests have high rates photosynthesis
Most carbon is sequestered for hundreds years
Most carbon is in the stem
Trees only a carbon sink for the first 100 yrs
Carbon sink
Something that absorbs more carbon than it releases
Aquifers
Permeable rocks such as chalk and sandstone
Groundwater is abstracted for public use from aquifers by wells and boreholes
Upper surface of saturation is a water table
Height fluctuates because of rainfall and drought
Artesian Basins
They are aquifers that have been confined between two impermeable rocks
They are under artesian pressure
Artesian aquifer when water flows to surface under its own pressure
London is an artesian basin
Water is trapped in London by clay and gault clay
Water table fell by 90cm as 19th centaury exploited water 1992 Thames water began to be abstracted
Use of fossil fuels
Global industrialisation and urbanisation
Dependant on fossil fuels
2013 87% of global energy consumption
10 billion tonnes year
3 stages of Carbon capture and store
CO2 separated from emissions
CO2 compressed and transported by pipelines
CO2 injected into porous rocks deep underground
How can carbon capture and store help?
Reduce greenhouse emissions by up to 90% in USA
Undergoing a pilot program in Scotland
High costs up to 1 billion
Requires storage reservoirs with certain geological conditions
Positive feedback
An initial change cause further change
Negative feedback
An initial change counters a system change which restores equilibrium
What does increase temp lead to in water cycle?
More evaporation
Atmosphere holds more vapour
Vapour is a greenhouse gas
Increases long wave absorption
High temperatures
What does lower temp lead to in water cycle?
More vapour
Increases long wave radiation
Greater cloud cover
More solar radiation reflected
Less solar radiation absorbed
Lower temp
What does increased atmospheric CO2 lead to?
Photosynthesis stimulated and CO2 moves to biosphere
Carbon moves to soil and ocean due to decomposition
Carbon moves to sediments
Becomes a carbon sink
What could global warming do to carbon cycle?
Intensify carbon cycle
Speed up decomposition
Release more CO2 to atmosphere
Methods of monitoring water/carbon
Satellites
Remote sensing
GIS means data can be mapped to show anomalies and trends
Diurnal changes
occur within 24 hr period
lower temp at night reduces evapotranspiration and stomata close so no CO2 taken in
Convectional precipitation is dependant on heating of the ground by sun
Seasonal changes
controlled by variations in solar radiation which peaks in June
Evapotranspiration highest in summer
Variation sin carbon are shown by NPP of vegetation
During summer trees are in full foliage
Phytoplankton stimulated by rise in temp in March
Glacial water cycles
Water from ocean reservoir to ice sheets and glaciers
sea level reduces 100m
glaciers are 1/3 of land mass
as ice sheets advance they destroy forest and grassland
reduced exchange between spheres
Glacial carbon cycles
reduction in atmospheric CO2
changes in ocean circulation bring nutrients to the surface and stimulate phytoplankton growth
CO2 in vegetation shrinks
Lower ocean temp means carbon dissolves more
How has human activity affected demand for water?
Larger demand for water
For agriculture and human supply
Creates water shortages
Overuse of aquifers in Bangladesh led to incursions of saltwater making it unfit for drinking
What has urbanisation caused in the water cycle?
Deforestation to make room for buildings
Reduced evapotranspiration
Lower water tables
Decreased throughflow
What does global warming lead to in the water cycle?
Increased evaporation
More water vapour
Raises global temp
Increases evaporation
What does global warming lead to in the carbon cycle?
Higher temperature
Increased decomposition
Accelerates carbon transfer from biosphere/pedosphere to atmosphere
Permafrost carbon released
Acidification of ocean stores
3 ways to protect carbon cycles
Wetland restoration
Afforestation
Agricultural practices
Wetland restoration
Freshwater marsh, salt marsh and peat land
Ground is permanently saturated
Contain 35% of carbon
destroying wetlands releases CO2 and CH4
Restoration raises water tables
Removing embankments means wetlands can be reconnected to rivers
Afforestation
Planting trees in deforested areas
trees are carbon sinks
reduces flood risk and soil erosion
protection from loggers, farmers and miners
REDD Reducing Emissions from Deforestation and Degradation
Projects established such as Amazonia
Agricultural practices
Overcultivation, overgrazing result in soil erosion
Releases large carbon to atmosphere
100 mil tonnes CH4 from livestock
Facts about Kyoto protocol
1997
Rich ACs agreed to legal binding CO2 restrictions
some of biggest polluters(China and India) exempt
USA and Australia refused to ratify the treaty
Facts about Paris Climate convention
2015
Reduce global CO2 emissions below 60% by 2050
Not legally binding
Rich countries assist poor countries with funds and technology
China/India argue Europe more responsible as past industrialisation has caused this
Cap and trade
Polluters cut emissions and pay remissions if they don’t
Allocated an annual quota for CO2
They receive carbon credits if they emit less which can be traded
Offsets are awarded to countries for afforestation
3 strategies for protecting water cycle
Forestry
Water allocations
Drainage basin plans
Forestry
Recognised by REDD, UN
Fund programs to protect tropical forests
50 partner countries funded
WWF
10% AMAZON BASIN covered by ARPA
Water allocations
governments allocate water resources
Agriculture consumers most water
Wastage occurs through evaporation
zero soil disturbance and drip irrigation stop the waste of water
loss to run off stopped by contour ploughing and vegetative strips
Drainage basin plans
Most effective water management
Good for adapting different needs of different places
Run off storage and groundwater is targeted
Run off controlled by reforestation and increasing permeable surfaces
Water storage improved by restoring wetlands