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Facts
CO2 concentration on the rise since Industrial Revolution
50% of planetary dry biomass is carbon
ESMs only created ~25 years ago
Sources
animals
plant matter
industry
deforestation
Sinks
atmosphere
ocean: 40,000 mGt of carbon
land biota, soil litter, peat: 2,000 mGt
Fluxes
photosynthesis 62 mGt
respiration and decomposition 60 mGt
physical and chemical processes
What happens to the CO2 we emit?
Sources
90% from industrial activity, 9.7 GtC/year
10% from land use change, 1.1. GtC/year
Sinks
48% in atmosphere, 5.2 GtC/year
29% in forests/plants, 3.2 GtC/year
26% in oceans, 2.9 GtC/year
4% imbalance
hard to estimate land stores because there is no mixing, unlike atmosphere and oceans
terrestrial carbon stores, 1995
Vegetation: 610 GtC
Soils 1580 GtC
Land Carbon Storage Patterns
storage of carbon greatest in wooded systems, worst in deserts
more carbon below ground in boreal forests
frozen, waterlogged soil, short growing period
Global Carbon Budget
fossil carbon grown as a source massively
does not match sources to sinks, area of research
Carbon Cycle on Land
gross photosynthesis
bole, root, microbial, litter, dark and photo respiration
CO2 storage
What makes the carbon budget change?
what makes photosynthesis and respiration change
resource supply and resource demand
Photosynthesis
6CO2 + 12H2O -> 6O2 + C6H12O6 + 6H2O
temperature, light, etc
the carbon that forests remove from the air is much more impactful than the oxygen they release
Respiration
6H2O + C6H12O6 + 6O2 -> 6CO2 + 12H2O + energy
respiration has a 1:1 correlation with temperature, not quite the same in nature
Calculating the carbon balance
carbon balance = total CO2 in - total CO2 out
Ways of thinking: models
terminology, description with words
mapping out a process with pictures
representing processes with numbers
all MODELS, need to use numbers to estimate quantities
terrestrial ecosystem process mapped with words: carbon cycle
or, more detailed with quantities
carbon is accumulatory
massive seasonal shifts in carbon sequestration
terrestrial biosphere changes with growing period, etc.
GPP high in Northern Hemisphere in their summer, low in their winter
forests highly sensitive to radiation changes
nitrogen also important
El Nino
massive effects on carbon balance
spikes in atmospheric CO2 increase during El Nino events
increase in fires in SEA (0.4 GtC 2011-2015)
decrease in Gross Primary Productivity (e.g. amount of carbon fixed by vegetation) in South America due to dryness
increase in respiration in East Africa due to warmth (0.6 GtC)
Policy Context
carbon stocks, land use change, and mitigating climate change
possible to manage increased carbon uptake from forests
be specific in where planting trees would do most good
REDD: UN policy to reduce emissions from deforestation and degradation
Houghton et al 2015, showed how investing in tropical forests would pull emissions down faster than just cutting fossil fuel usage