resp
coal, oil, gas
sedimentary rocks
soil organic carbon
food wars
plants
atmosphere
phytoplankton
food web
shellfish and corals
deep ocean sediments
deep ocean currents
ocean surface
carbon is stored in everything
cryosphere- 0.01,% soil in permafrost
lithosphere- 99.9%, sedimentary rocks, limestone (fossil fuels)
hydrosphere- 0.04%, deep dissolved, inorganic. small surface carbon
biosphere- plants and biological matter, soil.
atmosphere- 0.001%, co2 + methane
land | ocean | atmosphere |
---|---|---|
carbon cycle is responsible for the formation of soil. carbon in the form of oganic matter introduces important nutrients and provides structure for soil | carbon can be converted into calcium carbonate, which is used by some marine organisms to build shells | carbon dioxide in the atmosphere warms earth naturally through greenhouse effect |
carbon in the form of organic matter is essential for plant growth and food production | carbon cycle has an impact on photoplankton. basic food. phytoplankton consumes carbon dioxide during photosynthesis. carbon passed along food chain | increases in carbon emissions due to human activities (deforestation, combustion). lead to enhanced greenhouse effect. |
carbon stored in in grass provides fodder for animals | carbon stored by vegetation has significant effect on atmosphere, deforestation vs afforestation | |
carbon provides energy in the form of wood and fossil fuels |
volcanic eruptions
burning fossil fuels
respiration
ocean loss
decomposition
Photosynthesis
→ atmosphere/ biomass
→ energy from the sun. co2 + water = glucose and oxygen
→ plants grow
→ food chain, respiration, decomposition
Combustion
→ burning releases greenhouse gases
Ocean
→ carbon sink taken up by organisms, make limestone shells
→ ocean to the atmosphere also
Respiration
→ carbon from living organisms
→ glucose and oxygen break down to make co2 and water
Decomposition
→ dead biomass goes into the soil
Weathering
→ atmosphere to the hydrosphere
carbon + water = acid rain
chemical weathering on rocks
co2 in water to form calcium carbonate
Sequestration
photosynthesis
sequestration
chemical weathering
ocean uptake
water and carbon is essential for life
water is present in the atmoshere as water vapor, droplets and
carbon exists as methane and co2.
these are a natural ghg effect, prevents some energy from escaping into space and reflecting it back into earth. earth qould be frozen -18 without it
enhanced gh effect is caused by human activities causing an increase in the concentration of greenhouse gases in the atmosphere. reflects more energy back to the earth
wildfires:
rapidly transfer large quantities of carbon from biomass to the atmosphere. loss of vegetation decreases photosynthesis. long term it can encourage new plant growth. may have a neutral effect
industrial revolution.
1 hydrocarbon extraction and use (extraction and burning of fossil fuels releases co2)
fuel would say squestered in lithosphere for millions of years
2 deforestation
forests may be cleared for agriculture, logging or developments. clearance reduces size of carbon store.
3 farming practices
animals release co2
ploughing releases co2
rice growth can release methane
co2 from machinery
food is in demand
land use changes.
change of natural or agricultural urban land causes more carbon in atmosphere. vegetation removed. concrete production releases co2.
difference between inputs and outputs of carbon into a subsystem.
carbon source: releases more carbon than it can absorb (emits carbon)
carbon sink absorbs more carbon.
positive:
temperature rise → plant respiration rate increases → co2 in atmosphere increases → greenhouse effectincreases
negative
extra co2 in atmosphere increases → extra co2 causes plants to grow → plants remove and store co2 from atmosphere → co2 in atmosphere reduces
water:
temperature rise → evaporation increases → water vapour in atmosphere increases → greenhouse effect increases.
amount of water vapour in the atmosphere increases causing clouds to form → evaporation increases → temperature falls → increased cloud cover reflects more suns energy back to space.
individual:
→ use cars less, efficient or electric cars
→ homes can be made more energy efficient- eg, double glazing, insulation
national:
→ reduce reliance on fossil fuels for powering homes
→ investing in renewables
→ afforestation and restoration of forests to increase carbon uptake
→ sustainable developments, public transport
→ carbon capture and storage
global: international treaties to cut co2 emissions and set limits- Kyoto Protocol (1997) / Paris Agreement (2015)
carbon trading schemes limiting emissions by countries and allowing credits to be sold
carbon capture and storage
collecting carbon dioxide from emissions and then trapping it underground/water
its expensive and not always viable. unknown environmental umpacts
plantation forests:
the forests act as a sink. if the soft wood is used in non processed products, plantations can be more effective than natural woodland.
carbon is removed to allow more to be captured
space requirement, lack of biodiversity
land use change:
“carbon farming”
replacing crops with better carbon stores such as hay and oats
tilling the soil to prevent erosion and overly aerated microorganisms
“reduce deforestation”
only buy fsc wood and tree products
kyoto protocol clean development mechanism
grassland improvements
develop pedospheric sequesration
less soil erosion, grass pulls o2 into soil
avoid overgrazing
aviation advancement:
fuel efficient routes, avoid circling the airport before landing
minimise towing and taxiing
slower cuising speeds
aircraft to route, ensure all seats are occupied
improve aerodynamics, biofules, ccs, minimise weight
2005 kyoto protocol:
developed countries are the biggest contributors, heavier burden on them:
three mechanisms behind the protocol:
internations emissions trading. each county has a set quoto of emissions. they can trade it with other countries which remains an international limit
clean development mechanism- developed countries can earm more emissions if they implement a successful emission reduced project in a developing country
joint implementation- countries with a cap on the emissions can work together to reduce total emissions. they can earm more emissions
evaluation: generally a success. legally binding meant countries had to adhere
1990-2012 original kyoto protocol parties reduced co2 by 12.5% which was beyond the 2012 target.
this result is largely a result of the collapse of the SOviet Union, decline of russia industry. 42% emissions from USA and CHina- those who did not agree
2009 copenhagen accord
individual personal emission reduction targets for each country.
developing countries notified but not set caps.
developing countries worried the accords would replace kyoto protocol.
accord was not legally binding
these lacked the legally binding so it lacked power.
it did not cap developing countries which are the fastest growing emitters. however it did allow them to freely develop economically
deal unites us, china and other major developing countries for the first time. developed countries will aim to mobalise 100bn py by 2020, to address the needs of developing countries
2015 paris agreement
keep global temperature increase below 2* above pre-industrial
work against climate change and reduce ghg emissions in a way that doesnt threaten food production
paying suitable amounts of money for aid against climate change
not legally binding. each country provides its own targets- developed or otherwise
name and shaming of countries
1st agreement to unite all countries- caused conflict between developed and developing. south africa resulted in loss and damage because the agreement said developing countries would get aid from developed peers
200 billion trees, 15,000 species, 20% of world’s biomass is Carbon
9 countries, 5.5 million km squared. grown and retreated with ice ages
peru, brazil, bolivia, colombia
carbon:
80-120 billion tonnes
carbon sink of 1-3 gigatons/year
above ground, biomass store increases 0.3-0.5% year
rising productivity due to sequestration in atmosphere
2015 study said uptake by forest has halved and ovetaken by fossil fuel emissions from latin America
2 billion tons/ year in 1990, now 1 billion
carbin sink
concentration of co2 in atmosphere leads to increased uptake of trees, live quicker, but die sooner
water
175 thousand cumec discharge into atlantic per day. 15% of all freshwater entering oceans
Rio NEgro, 2nd largest river in terms of flow. 100m deep, 24km wide at mouth of Manaus in Brazil
2,300mm annual reainfall across whole basin. NW can be 6,000 half never reaches ground
48% evaporated and transpired, 30% reaches sea
drivers of change:
deforestation- 19,368 km over 8 years
brazil is the 4th largest climate polluter- 75% from deforestation and land use
59% from amazonion deforestation and burning
slash and burn techniques- humidity decreases in soil to only top metre
more water evaporates, previously held in canopy
albedo (reflectiveness) and temperature increases
soil porosity decreason, more erosion o sitting lakes and rivers
evaporation form shallow cumulus clouds which dont produce rain
salts and organic fibres are transpired by trees- forms condensation nuclei to encourage rainfall. deforestation makes rain less
forests absorb 11% of solar radiation.