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https://www.youtube.com/watch?v=Uat UDnFmNTYhttps://www.youtube.com/watch?v=Uat UDnFmNTY https://www.youtube.com/watch?v=x1S gmFa0r04https://www.youtube.com/watch?v=x1S gmFa0r04
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IPCC
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Sources: Petit et al (1999) Nature 399:429- 436 and IPCC(2000) Today 400 ppm CO 2 2 ppm CH 4 Atmospheric CO 2 has increased rapidly to levels above anything in Earth’s recent past 2100?
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IPCC
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http://www.iceuls.com/_photo/b.jpg
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Fossil Fuel and Cement Emissions Global fossil fuel and cement emissions: 36.1 ± 1.8 GtCO 2 in 2013, 61% over 1990 Projection for 2014 : 37.0 ± 1.9 GtCO 2, 65% over 1990 Estimates for 2011, 2012, and 2013 are preliminary Source: CDIAC; Le Quéré et al 2014; Global Carbon Budget 2014CDIACLe Quéré et al 2014Global Carbon Budget 2014 Uncertainty is ±5% for one standard deviation (IPCC “likely” range)
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Atmospheric Concentration The global CO 2 concentration increased from ~277ppm in 1750 to 395ppm in 2013 (up 43%) Mauna Loa registered the first daily measurements above 400pm in May 2013 Globally averaged surface atmospheric CO 2 concentration Data from: NOAA-ESRL after 1980; the Scripps Institution of Oceanography before 1980 (harmonised to recent data by adding 0.542ppm) Source: NOAA-ESRL; Scripps Institution of Oceanography; Global Carbon Budget 2014NOAA-ESRLScripps Institution of OceanographyGlobal Carbon Budget 2014
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Where Is The Carbon Going? Houghton et al. (2007) Ecosystem Carbon Sink
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Global Carbon Budget The cumulative contributions to the Global Carbon Budget from 1870 Contributions are shown in parts per million (ppm) Figure concept from Shrink That Footprint Source: CDIAC; NOAA-ESRL; Houghton et al 2012; Giglio et al 2013; Joos et al 2013; Khatiwala et al 2013; Le Quéré et al 2014; Global Carbon Budget 2014Shrink That FootprintCDIACNOAA-ESRLHoughton et al 2012Giglio et al 2013Joos et al 2013Khatiwala et al 2013 Le Quéré et al 2014Global Carbon Budget 2014
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Global Carbon Budget Emissions are partitioned between the atmosphere, land, and ocean Source: CDIAC; NOAA-ESRL; Houghton et al 2012; Giglio et al 2013; Joos et al 2013; Khatiwala et al 2013; Le Quéré et al 2014; Global Carbon Budget 2014CDIACNOAA-ESRLHoughton et al 2012Giglio et al 2013Joos et al 2013Khatiwala et al 2013 Le Quéré et al 2014Global Carbon Budget 2014
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Changes in the Budget over Time The sinks have continued to grow with increasing emissions, but climate change will affect carbon cycle processes in a way that will exacerbate the increase of CO 2 in the atmosphere Source: CDIAC; NOAA-ESRL; Houghton et al 2012; Giglio et al 2013; Le Quéré et al 2014; Global Carbon Budget 2014CDIACNOAA-ESRLHoughton et al 2012Giglio et al 2013Le Quéré et al 2014Global Carbon Budget 2014 Data: GCP
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The Great Ocean Pump –Physical pump (air-sea exchange) pCO2_atmosphere, pCO2_water, [CO2] –Chemical pump (inorganic CO2 chemistry) DIC, Alkalinity, and pH –Biological pump (photosynthesis and decomposition) DOC/DOM, DOC/POC
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Air-Sea Exchange
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http://www.awi.de/fileadmin/user_upload/Research/Research_Di visions/Geosciences/Glaciology/download_lecture_global_carbo n_cycle/pk1011_cc_05_dic.pdf Revelle factor = (Δ[CO2] / [CO2]) / (Δ[DIC] / [DIC])
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Ocean Carbon Cycle
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Ocean Sink Ocean carbon sink continues to increase 9.4±1.8 GtCO 2 /yr for 2004–2013 and 10.5±1.8 GtCO 2 /yr in 2013 Source: Le Quéré et al 2014; Global Carbon Project 2014Le Quéré et al 2014Global Carbon Project 2014 Individual estimates from Buitenhuis et al. (2010); Aumont and Bopp (2006); Doney et al. (2009); Assmann et al. (2010); Ilyiana et al. (2013); Sérérian et al. (2013); Oke et al. (2013); Landschützer et al. (2014); Park et al. (2010); Rödenbeck et al. (2014). References provided in Le Quéré et al. (2014). Data: GCP this carbon budget individual ocean models data products
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Nemani, 2003, Science
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Trends in NPP from Satellite
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Desai et al., 2006
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Terrestrial Sink The residual land sink is increasing with time to 9.2±1.8 GtCO 2 /yr in 2013, with large variability Total CO 2 fluxes on land (including land-use change) are constrained by atmospheric inversions Source: Le Quéré et al 2014; Global Carbon Project 2014Le Quéré et al 2014Global Carbon Project 2014 Individual estimates from Zhang et al. (2013); Oleson et al. (2013); Jain et al. (2013); Clarke et al. (2011); Smith et al. (2001); Sitch et al. (2003); Stocker et al. (2013); Krinner et al. (2005); Zeng et al. (2005); Kato et al. (2013); Peters et al. (2010); Rodenbeck et al. (2003); Chevallier et al. (2005). References provided in Le Quéré et al. (2014). Data: GCP this carbon budget individual land models atmospheric inversions (colours) this carbon budget individual land models fire-based estimate this carbon budget individual land models
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Anthropogenic Perturbation of the Global Carbon Cycle Perturbation of the global carbon cycle caused by anthropogenic activities, averaged globally for the decade 2004–2013 (GtCO 2 /yr) Source: CDIAC; NOAA-ESRL; Le Quéré et al 2014; Global Carbon Budget 2014CDIACNOAA-ESRLLe Quéré et al 2014Global Carbon Budget 2014 Data: CDIAC/NOAA-ESRL/GCP
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Land-Use Change Emissions Global land-use change emissions are estimated 3.3 ± 1.8 GtCO 2 during 2004–2013 The data suggests a general decrease in emissions since 1990 Three different estimation methods have been used, indicated here by different shades of grey Land-use change also emits CH 4 and N 2 O which are not shown here Source: Houghton et al 2012; Giglio et al 2013; Le Quéré et al 2014; Global Carbon Budget 2014Houghton et al 2012Giglio et al 2013Le Quéré et al 2014Global Carbon Budget 2014 Indonesian peat fires
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Source: NOAA ESRL
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s Source: Picarro, Inc. / Nathan Phillips, BU
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http://media-1.web.britannica.com/eb- media/75/135075-004-105F7745.jpg
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Observed Emissions and Emissions Scenarios Emissions are on track for 3.2–5.4ºC “likely” increase in temperature above pre-industrial Large and sustained mitigation is required to keep below 2ºC Over 1000 scenarios from the IPCC Fifth Assessment Report are shown Source: Fuss et al 2014; CDIAC; Global Carbon Budget 2014Fuss et al 2014CDIACGlobal Carbon Budget 2014 Data: CDIAC/GCP/IPCC/Fuss et al 2014
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+ Atmosphere 45% Oceans 26% Land 29% 9.9 Gt C yr -1 0.9 Gt C yr -1 2013 Le Quéré et al (2013) Photosynthesis Beer et al. (2010) Respiration Autotrophic Heterotrophic >120 Gt C yr -1 c.120 Gt C yr -1 Cumulative Atmosphere to Ocean CO 2 Flux (Gt C) Ocean Land Cumulative Atmosphere to Land CO 2 Flux (Gt C) Year Arora et al. 2013 Terrestrial Biosphere CO 2 Flux Dominates Carbon Cycle Prediction Uncertainty Ok Not Ok
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+ Atmosphere 45% Oceans 26% Land 29% 9.9 Gt C yr -1 0.9 Gt C yr -1 2013 Le Quéré et al (2013) Photosynthesis Beer et al. (2010) Respiration Autotrophic Heterotrophic >120 Gt C yr -1 c.120 Gt C yr -1 Cumulative Atmosphere to Ocean CO 2 Flux (Gt C) Ocean Land Cumulative Atmosphere to Land CO 2 Flux (Gt C) Year Arora et al. 2013 Terrestrial Biosphere CO 2 Flux Dominates Carbon Cycle Prediction Uncertainty Ok Not Ok Booth et al, ERL, 2012
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Buffam et al., 2011, GCB
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Terrestrial carbon cycle feedback is a leading order uncertainty for climate simulation IPCC AR5 WG1 CH6
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http://carboncycle.aos.wisc.ed u/carbon-budget-tool/
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