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Figure: 2 Theglobalcarboncycle Sea-to-airfluxofCO for1995 Earthsystemmodels&futureclimate

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IA C E T H

Institute for Atmospheric and Climate Science

Earth system models & future climate

Figure: IPCC, 2001

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 1 / 30

IA C E T H

Institute for Atmospheric and Climate Science

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

The global carbon cycle

[IPCC, 2007, Fig. 7.3]

natural fluxes (black); anthropogenic ones (red)

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 2 / 30

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Sea-to-air flux of CO

2

for 1995

[IPCC, 2007, Fig. 7.8]

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Temperature & salinity in surface waters

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 4 / 30

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Institute for Atmospheric and Climate Science

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Nutrients in surface waters

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 5 / 30

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Ocean carbon pumps

[IPCC, 2007, Fig. 7.10]

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Ocean carbon pumps

The ocean can alter atmospheric CO2concentrations through 3 mechanisms:

I Solubility pump: absorption or release of CO2 due to changes in solubility of gaseous CO2

I Organic carbon pump: changes in carbon fixation to POC in surface waters by photosynthesis and export of this carbon through sinking of organic particles out of the surface layer - this process is largely limited by availability of light and nutrients (P,N, silicic acid, iron)

I CaCO3counter pump: changes in the release of CO2in surface waters during formation of CaCO3 shell material by plankton (is only important on very long timescales)

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 7 / 30

IA C E T H

Institute for Atmospheric and Climate Science

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Linear trend of annual T

[IPCC, 2007]

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 8 / 30

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

T , sea level &

NH snow cover

(4)

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11 of the 12 last yeares rank among the 12 warmest years since 1850

[IPCC, 2007]

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 10 / 30

IA C E T H

Institute for Atmospheric and Climate Science

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Global dimming in Central Europe

[Behrens, 2003]

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 11 / 30

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Reconstructed temperatures

[IPCC, 2007]

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Reconstructed climate 125,000 years ago

[IPCC, 2007]

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 13 / 30

IA C E T H

Institute for Atmospheric and Climate Science

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 14 / 30

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Human vs. natural sources of GHGs

[IPCC, 2007]

(6)

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Radiative forcing components

[IPCC, 2007]

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 16 / 30

IA C E T H

Institute for Atmospheric and Climate Science

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Radiative forcing probability distribution

[IPCC, 2007]

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 17 / 30

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

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Observed vs. simulated T changes

[IPCC, 2007]

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 19 / 30

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Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Predicted future temperature changes

[IPCC, 2007]

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 20 / 30

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Predicted future temperature changes

[IPCC, 2007]

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Predicted future temperature changes

[IPCC, 2007]

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 22 / 30

IA C E T H

Institute for Atmospheric and Climate Science

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Predicted future precipitation changes

[IPCC, 2007]

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 23 / 30

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Expected changes in extremes

[IPCC, 2007]

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Changes in extremes

[IPCC, 2007]

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 25 / 30

IA C E T H

Institute for Atmospheric and Climate Science

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Changes in extremes

[IPCC, 2007]

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 26 / 30

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Current and projected CO

2

emissions

[N. Gruber, ETH]

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1920 1940 1960 1980 2000 2020 2040 2060 2080 2100 0

500 1000 1500 2000

Inventories and Cumulative Fluxes [PgC]

1920 1940 1960 1980 2000 2020 2040 2060 2080 2100 0

500 1000 1500 2000

Inventories and Cumulative Fluxes [PgC]

HADLEY MODEL: IS92a SCENARIO

Emissions

IPSL MODEL: SRES-A2 SCENARIO

Emissions

CARBON-CYCLE /

CLIMATE SYSTEM FEEDBACKS

Atmosphere

Atmosphere Ocean

Ocean

Land Land

Sarmiento and Gruber (2002)

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 28 / 30

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Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Biophysical feedback, land cover change

[A. Arneth, Lund, Sweden]

Ulrike Lohmann (IACETH) Earth system models & future climate June 21, 2007 29 / 30

Carbon cycle Observations Paleo Drivers Attribution Future Carbon&Future

Impact on temperature

[IPCC, 2007, Fig. 10.20]

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