what is carbon cycle
it is the complex procceses carbon undergoes as it is transformed from organic carbon (the form found in living organisms such as plants and trees) to inorganic carbon and back again
what are the most common carbon compounds?
carbon dioxide-atmosphere,oceans,soils
methane-atmosphere,oceans,soils,rocks
calcium carbonate-rocks,shells,oceans
hydrocarbons-coal,oil,gas
bio molecules-proteins carbohydrates
what is the primary source of carbon?
is the earths interior,it was stored in mantle when earth formed ,escaped from the mantle at constructive and destructive plate bpundaries as well as hotspots volcanoes
much of c02 released at destructive margins is derived from metamorphism of carbonate rocks subducting with the ocean crust
carbon is held as biomass in living and dead organisms
carbon is removed into lpngterm storage by burial of sedimentrary rock layers
lithosphere
includes the crust and the uppermost mantle(constitutes the hard and rigid outer layer of the earth
inorganic deposits of carbon in the lithosphere includes fossil fuels like coal, oil and natural gas , limestone
organic forms of carbon in the lithosphere include litter,organic matter and humic substances found in soils
hydrosphere
the ocean stores can be divided into three
the surface layer where sunlight penetrates so that photosynthesis can take place contains 900Gtc
intermediate and the deep layer (37,100Gtc)
living organic matter(30Gtc)
dissolved organic matter(700Gtc)
when organisms die their dead cells,shells and other parts sink into this deep water.decay releases c02 into deep water.some material sinks right to the bottom where it forms layers of carbon rich sediments
over millions of years chemical and physical processes may turn these sediments into rocks
biosphere
total sum of all living matter
main stores of carbon are
living vegetation
plant litter
soil humus-originates from litter decomposition
peat-accumulation of partially decayed vegetation or organic matter that is unique to natural areas called peatlands or mires
animals
atmospshere
despite its relatively small concentration co2 is a potent greenhouse gas and plays vital role in regulating the earths temperature also stroes methane
geological component
is where it interacts with the rock cycle in the processes of weathering,burial,subduction and volcanic eruptions
photosynthesis
phytoplankton in the sunlit durface waters of the ocenas as well as terrestrial plants,photosynthetic algae and bacteria,turn carbon into organic matter
they use sunlight energy to combine carbon dioxide from the atmosphere with water to form carbohydrates.these carbohydrates store energy
oxygen is the bi product
respiration
plants then use some of the stored carbohydrates as an energy source to carry out their life functions
decomposition
carbon stores in plants and aniamsl which die
dead plants and animals are decomposed by bacteria
carbon respores by decomposersinto the atmosphere
process leaves carbonin the spill
oceanic carbon pumps
water is able to dissolve c02
there is a negative correlation between temperature of the water and the amount of c02 that can be dissolved-leads to vertical deep mixing
combuation
occurs when organic material reacted (burned) in the presnece of oxygen to give off the products of co2,water and energy
biomass combustion
burning of living and dead vegetation
volcanic activity
rsnges from emissipn of gases,non explosive lava emissions to extremely violent explosive bursts that may last many hours
outline relationship between the water cycle and carbon cycle in the atmosphere
water is requires by plants to perform photosysnthesis
photosysnthesis moves carbon from the atmospjere to the bisphere
carbon dioxide mixes with water vapour to form acid
the process of respiration moves carbon and water from biosphere to the atmosphere
analyse the carbon sotres and transfers
lithosphere store is the largest carbon store 134,000 timedbigger thsn the smalles store(atmosphere)
atmosphere store is the smallest store but has the largest carbon transfer coming in and out where as lithosphere store gets the smallest amount of transfers measures per year even though it is the largest store
assess the magnitude of stores and flows in carbon cycle
the magnitude of carbon stores in the lithoshere is 2.5000 times larger than that stores in the atmosphere,hydrosphere and biosphere combines.carbon stores in the deep ocean is an outlier as it has 92% of all carbon not in lithosphere
explain changes in the global carbon cycle over long timescales
variations in the earths orbit and axis alter the amount of energy earth receives from the sun and leads to cycle of ice ages and warm periods
carbon dioxide in the atmosphere rose dramatically as temperatures warmed and different positive feedback mechanisms occurred to amplify this trend
asteroids also distrucpt the carbon cycle
northern hemisphere summers cooled and ice built up on land-this slowed the carbon cycle by reducing the rate of photosynthesis and respiration
cooler temperatures increased the amount of carbon transferred from the atmosphere to the ocean causing additional cooling
the global carbon cycle cannot exist without plant and the food webs they support
plants make their own food in the form of glucose sugar
heterotrophs do no photosynthesize and so must find and eat food made of carbon compounds such as proteins, carbohydrates and lipids, they break these complex organic compounds down into smaller molecules and use the carbon atoms to biosynthesize new organic carbon compounds
soil microbes,decompose dead material ,they break down larger compounds into smaller compounds-this process releases co2 to the surrounding soil to the atmosphere in the process called soil respiration -soil microbes move carbon down into the soil where it can be stores
the carbon cycle and carbon budget at plant scale
photosynthesis is the carbon cycle process that moves carbon atoms from the air into trees and all other plants. Carbon atoms move into the biosphere and into most food webs via this process
respiration-is is the key carbon cycle process that moves carbon atoms out of plants into the atmosphere, surrounding soil and water
biosphere-key carbon process that generates gains in biomass. Net primary production is a measure of the amount of carbon stored mostly as biomass
if the carbon input from photosynthesis is greater than the carbon output from respiration, trees will biosynthesize more biomass resulting in greater carbon storage. The measure of NPP will be higher. Conversely, if the carbon output of respiration is greater than the carbon input of photosynthesis, less carbon will be stored and measures of NPP will be lower.
example of a positive feedback cycle
the increase of the greenhouse gas carbon dioxide increases the earth’s surface temperature, warming the atmosphere. A warmer atmosphere,combined with drought in some forests,has been creating conditions for increased pine bark beetle infestations. the beetle infestation kills more trees which then dry out, dead trees are fuel for more wildfires as they burn wildfires release greenhouse gases such as CO2 increasing the temperature
carbon budget
balance between inputs and outputs
what is the main impact of the changing budget on the land?
increased temperatures has warmed up the land.areas warming of the land increases the rate of decay of accumulated dead organic matter leading to release of methane.Thaws permafrost 1672Gtc of carbon
what is ocean acidification
dissolving carbon dioxide in the ocean creates carbonic acid ,the ph of the oceans surfaces have dropped by 30%
therefore thinner and more fragile shells
reef loss due to carbonate ions
its not that significant
ocean warming
warming of the oceans as temperatures rise-decreases phytoplankton which could limit oceans ability to take carbon from the atmosphere though biological pump
more c02 means more phytoplankton
what is the main impact of changing carbon budget on cryosphere?
it is melting-retreat at 12.8% per decade
nighlty reflective ice is replaced by more heat absorbent water,when it starts to melt40% loss of arctic sea ice in 35 yrs
ocean absorbs more sunlight
positive feedback mechanism
ocean salinity
higher levels of precipitation (dilutes)
higher temperatures melt ice(dilutes)
weskens thermo-haline circulation and therefore the oceanic carbon pump
positive
what is sea level rise
thermal expansion (warmer oceans have greater volume)
predicted to increase 0.8 to 2m 2100
melting terrestrial ice -greater increase in fresh water entering ocesns than water lost due to evaporation
what is the main impact of changing carbin budget
enhanced green house effect-causing radiactive forcing
current radiative forcing 800 terawatts. predicted temperature increase of 1.5oc between 2030 and 2050
driver feedback in hydrosphere ,weakening thermohaline circulation and biosphere-wildfires
assess the impications of changes to the climate budget
enhanced greenhouse gases effect which leads to weakened thermon -this has powerful positive feedback
-permafrost
-ice melt
-disrupt the circulation
ocean acidification is an example of a less concern it is bad for crustation but weak feedback at global scale
therefore implication associated with positive feedbacks are most cncerning
environmental sequestration
afforestation
peat bogs-carbon does not decompose in peat therefore an important store
wet and restoration-carbon stored at saturation slows decay
technological sequestration
iron fertilisation-add iron rich dust to oceans which encoursges phytoplankton growth
urea fertilisation-add urea to ocean to encourage pyhploanton growth
carbon capture and storage-extract co2 from the air pump it underground
assess the environmental and technological sequestration methods
environmental
+ proven , measurable costs and benefits and aesthetically pleasing
- requires land(low value compared to urbanisation,agriculture and industry,slow,biosphere storage not as long
technological
+ compatible with current high-consumption lifestyles and capitalism
- unproven, possible unintended consequences, requires subsidy
solutions to climate change and its challanges
technological sequestration-unproven technology,delays shift away from fossil fuel economy
reduce meat and dairy as well as food waste-needs change from people very hard to enforce it on people
green taxes-not popular,more money people need to spend
using electric vehicles and hydropowered transport-need political agreement and there has only been one successful e-journey
global agreement unfccc-expensive and hard to get everyone to agree
aviation-we love cheap flights
where is carbon involved in the water cycle
animals respire
plants photsynthesis
water rewuires for decomposition
carbon compounds tranferred to ocean via water cycle flows
water vapour dissolved caebon dioxide to create carbonic acid
increased carbon dioxide enchande greenhouse effect,increasing humidity in the atmosphere
carbon get frozen and stored in ice caps
calcium carbonate flux to deep oceans
carbon absorbed by ocean taken to deep oceans by carbon pump,ocean respires .carbon in tropics after centuries
carbonic acid weahters carbonate rocks
outline the relationship between the water cycle and carbon cycle in the atmosphere
increasing concentration of carbon in the atmospshere has a warming effect on the planet and leads to increased evaporation
this can increase rates of precipotation or equally higher rates of evaporation can further exacerbate aridity
photsynthesis requires both precipitation and carbon dioxide
decomposition releases carbon dioxide and requires the presence of water-may link to melting of permafrost
water and carbon cycle positive feedback
increasing atmospheric carbon increases global air temperatures
increase in sea surface temperatures
release of methane crystals on the ocean bed
increased atmospheric methane concentrations
water and carbon negative feedback
increasing atmospheric carbon increases global air temperatures
increased ice melt and release of freshwater into the arctic ocean decreasing its salinity and increasing its temperature and density
ocean conveyor could weaken meaning that warm ocean currents such as the Gulf Stream weaken and do not transfer heat from the equator to the higher latitudes
processes in the water cycle that have a relationship with factors driving change in the carbon cycle
evaporation,precipitation-photosynthesis, and respiration (plant growth)
precipitation-respiration (carbonic acid water vapour and CO2)
precipitation-weathering(carbonic rocks)
precipitation,infiltration-photosynthesis,decomposition (soil formation)
evaporation,precipitation-combustion(wildfires)
to what extent does an understanding of feedback systems in the carbon cycle help attempt to mitigate impacts of climate change
feedback cycles describe the process where a change in a system leads to a cyclical sequence of changes which either accelerate or reverse the original change the system is dynamic equilibrium, understanding positive feedback can help mitigate climate change impacts
e.g deforestation which releases carbon in the atmosphere as forests are turned from carbon sinks into carbon sources, this will increase the impact of climate change as it leads to greenhouse effect
climate change has had several impacts on the carbon cycle as climate change has arisen from ghg emissions, resulting in the increased magnitude of carbon in the atmosphere, understanding feedback systems can largely help design mitigation actions but on its own, it doesn’t means mitigation will occur.
understanding negative feedback can help mitigate against climate change
e.g in the a,azon forest the increase in emissions has resulted in more productivity and encouraged faster growth resulting in my photosynthesis, absorbing more carbon. this can help suggest methods such as afforestation to reduce the impacts of climate change
outline how changes to the water and carbon cycles impacts the tropical rainforest environment
deforestation will release more carbon into the atmosphere which will enhance greenhouse effect
will increase temperature. if it increases by 2-3% 75% of Amazon will die off-longer dry seasons which will increase the risk of wildfires
deforestation and conversion to pasture reduce the volume of dead organic matter therefore reducing transfers to the soils and lithosphere by decomposition(lower levels of soil organic carbon
outline feedback between the water and carbon cycle in tropical ranforests
incfeasing atmopsheric carbon increases global air temperatures
mass death of tropical rainforests due to increased drought in tropics
increased decomposition of and release of carbon dioxide
deforestation is reducing evapotranspiration which means the atmosphere becomes less humid and this could reduce rainfall,increasing the risk of drought.few trees remain,interception of rainfall or evaporation off leaves is reduced,further reducing evapotranpiration.risk of drought also increased due to inhanced ghg effect ,there have been two major droughts in the past 10 years
with fewer trees,most rainfall reaches the ground immediatley
relationships between the water cycle and carbon cycle
high temperature-high precipitation/infiltration-high rate of photosynthesis-evapotranspiration as there is more plant growth-high precipitation
high precipitation-high rate of infiltration and throughfall-extesive overland and channel flow-weathering of carbonate rocks -carbon in water-consumers in heterotrophs
rank order the extent of human impacts on the water and carbon cycle
deforestation(20% since 1972)-reduces evapotranspiration,overland flow removes top soil so less infiltration and throughflow.Less photosynthesis therefore less carbon removed from the atmosphere and dead organic materials in soils
mining is large but local(10% of deforestation but concentrated )vegetation clearance which reduces evapotranspiration and convection rainfall.creates large man made stores e.g dams .less photosynthesis
agricultural practices-80% deforestation for cattle ranching,only 100000 hectares for palm,soy cultivation leads to soil compaction increading surface run off.Grassland and palm plantations reduced evapotrans.40% of regions ghg emmission are methane from cattle ranching
climate-ippc predicts dry seasons 3 weeks longer,increases incidents of weather extremes-more intense rainfall prolonges drought,photsysnthesis declines when forest flooded,combustion from it add carbon to the atmosphere
stretegies to mitigate the environmental change in the amaxon tropical rainforest
establishing clear property rights overland-the brazilian governemtn is keen to reduce land grabbing and illegal logging and ranching-not gonna solve the problem
ecotourism protects rainforests from hunting logging and mining and provides local employment.the posada amazonas lodge in the peruvian amazon for example is jointly run by an eco tour operator-not a large scale solution
encouraging markets to buy forest products from legally registered sources.The problem however is that the destination of many tropical commodities is often markets which are not eco sensitive for example amaxon rainforest timber is sold in china and india while brazilian beef is exported to russia-long term and great potential but how likely?
paying owners not to cut down the trees.the main international effort to reduce forest clearence known as redd and its based on that rich countries should pay poor countries not to cut down trees.4.5 billion was pledged-large scale ,great potential but requires investmwnt and long term commintment
monitoring deforestation using satellites and aeroplanes which can detect large scale illegal clearence-large scale great potential but requires investmwnt and long term commitmnt
what have they been doing to save brazilian rainforest
near real time monitoring system
700 people arrested
cut finance fore deforestation
share respnsibility in the chain of custody
50 million hectares protected
create protected areas
what are the successes
8.7 million hectares saved
stops 3 billion tones of co2 being emitted
managed a growing economy at the same time as reducing deforestation
what concerns still exist
15% of c02 emission results from deforestation
warming climate has led to beatle infestation
need to limit warming to 2c
budget of emission of 1bt of c02 until end of century-need to go down to 1 bt
5 ideas for the future
measure where,when and who is transmitting c02
disconnect development from carbon emission
share responsibility between government,busness,civil society