Water & Carbon Cycles
Water Cycle
Carbon Cycle
Indonesia Case Study
Deforestation
Palm Oil Industry
Set to increase, therefore deforestation will continue
Higher yield than other oil based crops
85% of palm oil is produced in Malaysia and Indonesia
Impacts on carbon cycle
Impact on water cycle
Trees no longer able to absorb CO2 via photosynthesis
Enhanced greenhouse effect
Resulting in global warming, ice melt, and sea level rise
Peat soils act as a carbon sink but upon exposure to air due to deforestation, they will release CO2 and can no longer act as a carbon store
Burning trees releases CO2 into atmosphere
Breaks the water cycle, reduction of rainfall so area becomes drier.
Drier conditions can increase the risk of forest fires, which release even more CO2 into atmosphere (positive feedback loop)
Surface flow is more rapid -----> ground becomes drier and more rapid soil erosion. Hard to grow crops, so animals and people will struggle to find food
Forest fires
Nearly all human caused as environment is too moist to ignite naturally
Caused the largest increase in atmospheric carbon since the 1950's
Atmospheric Cycle
Oceanic Cycle
Terrestrial Cycle
Carbon is cycled relatively rapidly between soil and vegetation and the atmosphere. "Fast carbon cycle"
Occurs within ecosystems, which are now almost all subject to intensive human impacts
Uptake of CO2 from atmosphere by plant photosynthesis. CO2 released back into atmosphere due to respiration of plants and animals
Land use changes and other human impacts have the potential to change the terrestrial carbon cycle
Carbon is held in dissolved form in the waters and in the tissues of ocean dwelling organisms
Primary inputs and outputs are by gas exchange with the atmosphere but also a significant input of both organic carbon and carbonate ions from continental runoff
Oceans are a very significant store of carbon
Carbon flux within oceans is controlled by physical, chemical, and biological processes
Carbon lasts up to 50 years in atmosphere while methane only lasts 12 years
Carbon and Methane
CO2 is relatively unreactive and and usually removed from atmosphere through interactions with the terrestrial and oceanic carbon cycles