Forest and Grassland Carbon in North America

A Short Course for Land Managers

Chris Swanston | An Introduction to the Carbon Cycle and Ecosystem Interactions: Global and Regional Trends

[+] Slides

The Global Carbon Cycle

Chris Swanston
U.S. Forest Service

Learning Objectives

Address some key questions:

Carbon Terms and Units

... boring, but useful ...

Common units of carbon stocks...

Carbon Terms and Units

... boring, but useful ...

Common units of carbon stocks...

Common units of carbon fluxes...

Carbon Terms and Units

... boring, but useful ...

Common units of carbon stocks...

Common units of carbon fluxes...

Common units of carbon density...

Global Carbon Distribution

Soil and vegetation

Soil and vegetation
UNEP World Conservation Monitoring Centre; www.carbon-biodiversity.net

Global Carbon Distribution

Live above- and below ground vegetation

Live above- and below ground vegetation
Ruesch and Gibbs, 2008

Global Carbon Distribution

Soil organic carbon to 1 meter depth

Soil organic carbon to 1 meter depth
USDA NRCS, 2000; www.soils.usda.gov/use/worldsoils

Global Carbon Distribution

Soil and vegetation

Soil and vegetation
UNEP World Conservation Monitoring Centre; www.carbon-biodiversity.net

Global Carbon Stocks

Carbon in soil and vegetation

Carbon in soil and vegetation
Mg = 1 million grams =1 metric ton
Pg = 1 billion metric tons

Global Carbon Stocks

Billion tons of Carbon (GTC)

Global Carbon Stocks
Data sources: Boden et al. 2011, Friedlingstein et al. 2010, Houghton 2007, IPCC 2007, Tarnocai et al. 2009.
1~ 2300 = Vegetation (550±100) and soils to 1m (1600-2000). Soils to 3m = 2300.
2 Industrial emissions from fossil fuels and cement, dating 1751-2008.
Figure modified from Climatesafety.org

Global Carbon Fluxes

Forest carbon balances (MtCO2), 1855-2000.

Forest carbon balances (MtCO2), 1855-2000.
MtCO2 = 1 million metric tons CO2

Global Carbon Fluxes

Net sources and sinks

Net sources and sinks
Global Carbon Project, 2010
Friedlingstein et al., 2010

Global Carbon Fluxes

Net sources and sinks

Net sources and sinks
Global Carbon Project, 2010
Friedlingstein et al., 2010

Fate of Anthropogenic CO2 (2000-2009)

Fate of Anthropogenic CO2 (2000-2009)
Global Carbon Project, 2010; www.globalcarbonproject.org

Then What?

Learn more about

...by watching the following presentations in this series

Thank You!

Questions and Answers

On the global carbon stocks slide the annual fossil fuel emissions pool looks small relative to the others. Why is that important and how is that pool growing relative to others?

Annual fossil fuel emissions are growing much faster than the other pools. It is important because that pool essentially comes from outside of the system in addition to the carbon cycle. There are natural additions from that pool into the carbon cycle but they are on the order of .1 gigatons a year. Now we are adding 7.7 gigatons of carbon per year. Even though there are some land and ocean sinks there is still an annual net increase of 4 gigatons every year and that is why we are seeing the concentration of carbon dioxide and other greenhouse gases rising in the atmosphere.

Questions and Answers

Can you tell us a little bit more about the interaction between carbon in the ocean and carbon in the atmosphere?

What we see in that surface component of the ocean acts in a much larger way with the atmosphere. In general we have about 92 gigatons of carbon coming into the ocean and only about 90 coming back which is approximately a 2.5 gigaton net sequestration of carbon in the ocean. Much of that is converted to bicarbonate once dissolved into the ocean. Because of the way it interacts chemically in the ocean, it causes acidification which has a deleterious effect on many different forms of life in the ocean. So as we increase the carbon dioxide the atmosphere it increases the pressure of moving that particular compound into the ocean. Acidification will increase for some time just as carbon dioxide is expected to increase for some time.

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