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Terrestrial biosphere and global change: the carbon cycle at the land surface Han Dolman [ dola@geo.vu.nl] dola@geo.vu.nlAlterra Wageningen, NL
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Bottom up: forest inventories, models Top Down: atmospheric methods The Dual constraint approach for carbon balances
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The Global Carbon Cycle Atmosphere 750, + 3 per year 1 -1.5 Deforestation 60 62 - 63 6.5 92 90 Terrestrial production & respiration Fossil fuels & cement production Oceanic exchange Terrestrial ecosystem Vegetation 610 Soils1400 Litter 60 _____________ Total2070 Surface ocean 1020 Marine biota 3 DOC 700 Ocean 38,100 Sediment 0.4 Fossil fuel reserves 4000 Carbonate rocks 65x10 6 4050100 92 6 6 4 0.2
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Interannual variability
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A global network
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Brasil: LBA-EUSTACH Sites Manaus K34 and Manaus C14 Caxiuana Rebio Jaru Fazenda Nossa Senhora
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Towers at Reserva Biologica do Rio Jaru ‘Abracos’ New tower
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CO 2 eddy fluxes over 2 years in the Central and Southern Amazon Data are 10-day averages. Missing data are green or dark blue
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Manaus: slight sesaonality
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Rebio Jaru: Seasonality
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Annual C-uptake in the Amazon
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Monthly NEE Loobos
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Interannual variability in NEE Loobos
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What is causing the variation in NEE? Radiation load Length of growing season
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Growing season length
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Conservation between carbon and water fluxes (WUE)
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Coupling of H 2 0-CO 2 flux at ecosystem level
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The Carbon Balance of a Forest
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Land Use Change
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Flask sampling Weather Fossil fuel emission Biospheric uptake Flux aircraft Free troposphere CO2 Landscape scale monitoring m C/dt+uM m C/ x+vM m C/ y = (C i -C m )/ t -W i ) I / m -A-R+M m C f / t
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Future: regional integration?
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CarboEurope - Flux Monitoring Sites 32 eddy correlation flux measurement towers 8 sites with process studies 5 with aircraft CO 2 profiles 7 chronosequences In addition (not shown): 10 stations of background atmospheric CO 2 monitoring plus 10 stations from NOAA / CMDL
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