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Mass Balancefor the carbon cycle    Robert MacKay    Clark College and Washington State    University Vancouver, WA
Camping
Student Learning Goals   Use a model to estimate the future concentrations of carbon dioxide    under several different a...
http://serc.carleton.edu/introgeo/mathstatmodels/examples/MassBalance.htmlhttp://serc.carleton.edu/introgeo/teachingwdata/...
From page 212 IPCC “Climate Change 2007 The Physical Science Basis”
IPCC 2007 Figure 7.3
IPCC 2007 Figure 7.3The Global Carbon Cycle for the 1990s . Red anthropogenic black preindustrial.From the diagram above, ...
IPCC 2007 Figure 7.3The Global Carbon Cycle for the 1990s . Red anthropogenic black preindustrial.From the diagram above, ...
IPCC 2007 Figure 7.3The Global Carbon Cycle for the 1990s . Red anthropogenic black preindustrial.From the diagram above, ...
IPCC 2007 Figure 7.3The Global Carbon Cycle for the 1990s . Red anthropogenic black preindustrial.From the diagram above, ...
Basic ModelWhat’s missing fromthis carbon cyclemodel?
Basic ModelWhat’s missing fromthis carbon cyclemodel?Rock (Lithosphere)and Humans
[ CO2 ]t +1 = ( A0,t + a0 St ) + ( A1,t e−1 / τ1 + a1 * St ) + ( A2,t e−1 / τ 2 + a2 * St ) + ( A3,t e−1 / τ 3 + a3 * St )...
Model and preliminary assignment   http://www.atmosedu.com/physlets/GlobalPollutio
Conclusion   The model can be used in an interactive lecture    discussion or as an assignment.   Implements the 2007 IP...
Using a Mass Balance Model to Understand Carbon Dioxide and its Connection to Global Warming
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Using a Mass Balance Model to Understand Carbon Dioxide and its Connection to Global Warming

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Using a Mass Balance Model to Understand Carbon Dioxide and its Connection to Global Warming

  1. 1. Mass Balancefor the carbon cycle Robert MacKay Clark College and Washington State University Vancouver, WA
  2. 2. Camping
  3. 3. Student Learning Goals Use a model to estimate the future concentrations of carbon dioxide under several different assumed emission scenarios. Learn how different carbon dioxide emission scenarios influence our best prediction of future global temperatures. Learn how a mass balance model applies to the global atmosphere. Calibrate a model with recent observations. Understand the sluggishness of the carbon cycle to anthropogenic changes. Synthesize results into a well written summary. Accurately read graphical information. Read and interpolate data from a table of values.
  4. 4. http://serc.carleton.edu/introgeo/mathstatmodels/examples/MassBalance.htmlhttp://serc.carleton.edu/introgeo/teachingwdata/examples/CFCsModel.htmlhttp://serc.carleton.edu/quantskills/activities/co2_global.html
  5. 5. From page 212 IPCC “Climate Change 2007 The Physical Science Basis”
  6. 6. IPCC 2007 Figure 7.3
  7. 7. IPCC 2007 Figure 7.3The Global Carbon Cycle for the 1990s . Red anthropogenic black preindustrial.From the diagram above, estimate the fraction of total anthropogenic carbon emissionsthat are attributable to land use changes.
  8. 8. IPCC 2007 Figure 7.3The Global Carbon Cycle for the 1990s . Red anthropogenic black preindustrial.From the diagram above, estimate the fraction of total anthropogenic carbonemissions that are attributable to land use changes.1.6/(8.0)=0.20 =20%
  9. 9. IPCC 2007 Figure 7.3The Global Carbon Cycle for the 1990s . Red anthropogenic black preindustrial.From the diagram above, estimate the fraction of all carbon emitted from humanactivity that is still in the atmosphere.
  10. 10. IPCC 2007 Figure 7.3The Global Carbon Cycle for the 1990s . Red anthropogenic black preindustrial.From the diagram above, estimate the fraction of all carbon emitted from humanactivity that is still in the atmosphere.165/(244+39)=58%
  11. 11. Basic ModelWhat’s missing fromthis carbon cyclemodel?
  12. 12. Basic ModelWhat’s missing fromthis carbon cyclemodel?Rock (Lithosphere)and Humans
  13. 13. [ CO2 ]t +1 = ( A0,t + a0 St ) + ( A1,t e−1 / τ1 + a1 * St ) + ( A2,t e−1 / τ 2 + a2 * St ) + ( A3,t e−1 / τ 3 + a3 * St ) IPCC 2007 page 213 τ 0 = infinite a0=0.217 a1=0.259 τ 1 =172.9 a2=0.338 τ 2=18.51 a3=0.186 τ 3=1.186Introduction to multi-box models (lecture notes)http://www.atmosedu.com/WSU/esrp310-550/notes/BoxModels/MatrixPractice1.pdf“Normal modes and the transient response of the climate system” , GRLMacKay and Ko, 1997 (http://www.atmosedu.com/WSU/esrp310-550/OceanModel.pdf )
  14. 14. Model and preliminary assignment http://www.atmosedu.com/physlets/GlobalPollutio
  15. 15. Conclusion The model can be used in an interactive lecture discussion or as an assignment. Implements the 2007 IPCC carbon impulse response function. Captures both the fast response and the sluggishness of the carbon cycle. Helps students understand how policy changes today have limited short term (20 yr) influence but important long term (60 yr) influence. Gives students more practice using graphical information. Open ended questions allow student to think for themselves.

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