1.1.3 The Carbon Cycle (global) Flashcards
Carbon Sink
any store which takes in more carbon than it emits e.g. intact/virgin tropical rainforest
Carbon source
any store that emits more carbon than it stores e.g. a damaged tropical rainforest
Main carbon stores (in order of magnitude)
1 Marine sediments and sedimentary rocks 2 Oceans 3 Fossil Fuel Deposits Soil Organic Matter 4 Atmosphere 5 Terrestrial Plants
Marine Sediments and Sedimentary Rocks
Lithosphere - Long-term
Easily the biggest store. 66 - 100 x10^18 metric tons of carbon. The rock cycle and continental drift recycle the rock over time, but this may take millions of years.
Oceans
Hydrosphere - Dynamic
The second biggest store contains a tiny fraction of the carbon of the largest store. 38 x10^12 metric tons of carbon. The carbon is constantly being utilised by
marine organisms, lost as an output to the lithosphere, or gains as an input from rivers and erosion.
Fossil Fuel Deposits
Lithosphere - Long-term but currently dynamic
Fossil fuel deposits used to be rarely changing over short periods of time, but humans have developed technology to exploit them rapidly, though 4 x10^12
metric tons of carbon remain as fossil fuels.
Soil Organic Matter
Lithosphere - Mid-term
The soil can store carbon for over a hundred years, but deforestation, agriculture and land use change are affecting this store. 1.5 x10^18 metric tons of carbon
stored.
Atmosphere
Dynamic
Human activity has caused CO₂ levels in the atmosphere to increase by around 40% since the industrial revolution, causing unprecedented change to the global climate. 0.75 x10^18 metric tons of carbon stored.
Terrestrial Plants
Biosphere - Mid-term but very dynamic
Vulnerable to climate change and deforestation and as a result carbon storage in forests is declining annually in some areas of the world. 0.56 x10^18 metric tons of
carbon.
Which sphere is the main store of carbon?
Lithosphere.
How are the stores distributed?
Unevenly. Oceans are larger in S hemisphere and biosphere storage mostly occurs on land. Terrestrial plant storage is focussed in the tropics and N hemisphere.
How are forests changing?
Declining in tropical areas in S hemisphere. Growing in N hemisphere.
Non-tropical forests…
have seen an increase in carbon sequestration in recent years, especially in Europe and Eastern Asia, due to conversion of agricultural land and plantations to new forests.
Forests in industrialised regions…
are expected to increase by 2050 but in the global
south, forested areas will decrease.
Rate of forest loss…
has decreased