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Published byBridget Bell Modified over 6 years ago
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The bottom-up approach
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Soils Network
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active associated sites
Eddy Flux network main flux sites active associated sites total coniferous 12 11 23 deciduous 8 3 evergreen broadleaf 4 2 6 mixed coniferous/ 1 crops 9 16 25 grassland 15 50 41 91
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Zanchi et al. in press
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Ciais et al., 2008
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Magnani et al., 2007
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Harrison et al., 2000
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Kutsch, Rebmann, unpublished
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Janssens, Ciais, Luyssaert and Schulze, unpublished
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at canopy level GPP is very similar Janssens, Ciais, Luyssaert and Schulze, unpublished
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grassland > forest Janssens, Ciais, Luyssaert and Schulze, unpublished
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other GHGs balance the grassland sink increase cropland losses Janssens, Ciais, Luyssaert and Schulze, unpublished
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forest biomass sink not secure Janssens, Ciais, Luyssaert and Schulze, unpublished
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The top-down approach
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Atmospheric network
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Figure: M. Heimann
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The European GHG balance
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GHGs add 10% to GWP
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ecosystems compensate 10% of fossil and other fluxes the N2O flux is as large as the forest sink
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the entire European sink is in Eastern Europe
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Conclusions The GHG balance of EU-25 is zero The Euopean GHG sink is located in eastern Europe We cannot study the carbon cycle in isolation. We have to seriously take the N-cycle on board
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