Why Global Warming Will Cross a Dangerous Threshold in 2036
 Posted: Mon Sep 29, 2014 7:17 am
Posted: Mon Sep 29, 2014 7:17 amWhy Global Warming Will Cross a Dangerous Threshold in 2036 
[ http://www.scientificamerican.com/artic ... d-in-2036/ ]
 
Emitting carbon dioxide at current rates will soon push Earth’s temperature up by 2 degrees Celsius. Here’s how to make the calculation yourself
 
Mar 18, 2014 By Michael E. Mann
If the world continues to burn fossil fuels at the current rate, global warming will rise 2 degrees Celsius by 2036, crossing a threshold that many scientists think will hurt all aspects of human civilization: food, water, health, energy, economy and national security. In my article "False Hope" in the April 2014 Scientific American, I reveal dramatic curves that show why the world will reach this temperature limit so quickly, and also why the recent slowdown in the rate of temperature increase, if it continues, will only buy us another 10 years. [ http://www.scientificamerican.com/artic ... d-by-2036/ ]
These numbers come from calculations made by me and several colleagues. We plugged values of Earth’s “equilibrium climate sensitivity”—a common measure of the heating effect of greenhouse gases—into a so-called energy balance model. Scientists use the model to investigate possible climate scenarios.
You can try this exercise yourself. The text below explains the variables and steps involved. You can download the climate data here and the model code here. And you can compare your results with mine, which are here. You can also change the variables to see what other future scenarios are possible. One note: the model runs on MatLab software, which can be obtained here.
We employed a simple zero-dimensional Energy Balance Model (“EBM”—see references 1 through 5 below) of the form:
[ http://www.scientificamerican.com/artic ... d-in-2036/ ]
REFERENCES
1. North, G. R., Cahalan, R. F. & Coakley, J. A., Energy balance climate models, Rev. Geophys. 19, 91–121 (1981).
2. Crowley, T. J. Causes of climate change over the past 1,000 years. Science 289, 270–277 (2000).
3. McGuffie, K. & Henderson-Sellers, A., A Climate Modeling Primer, 2nd Edition, Wiley, (1997).
4. Mann, M. E., Fuentes, J. D., Rutherford, S., Underestimation of Volcanic Cooling in Tree-Ring Based Reconstructions of Hemispheric Temperatures, Nature Geoscience, 5, 202–205 (2012).
5. Mann, M. E., Rutherford, S., Schurer, A., Tett, S.F.B., Fuentes, J. D., Discrepancies between the Modeled and Proxy-Reconstructed Response to Volcanic Forcing over the Past Millennium: Implications and Possible Mechanisms, J. Geophys. Res. 118, 7617-7627, doi:10.1002/jgrd.50609 (2013).
6. Wigley, T. M. L. & Raper, S. C. B., Natural variability of the climate system and detection of the greenhouse effect. Nature 344, 324–327 (1990).
7. IPCC, 2007: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [S. Solomon, D. Qin, M. Manning, Z. Chen, M. Marquis, K. B. Averyt,
M.Tignor and H. L. Miller (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA.
8. Myhre, G., Highwood, E. J., Shine, K. P. & Stordal, F., New estimates of radiative forcing due to well mixed greenhouse gases, Geophys. Res. Lett. 25, 2715-2718, 1998.
9. Ammann, C. M. et al., Solar influence on climate during the past millennium: Results from transient simulations with the NCAR Climate System Model. Proc. Natl. Acad. Sci. 104, 3713–3718 (2007).
			[ http://www.scientificamerican.com/artic ... d-in-2036/ ]
Emitting carbon dioxide at current rates will soon push Earth’s temperature up by 2 degrees Celsius. Here’s how to make the calculation yourself
Mar 18, 2014 By Michael E. Mann
If the world continues to burn fossil fuels at the current rate, global warming will rise 2 degrees Celsius by 2036, crossing a threshold that many scientists think will hurt all aspects of human civilization: food, water, health, energy, economy and national security. In my article "False Hope" in the April 2014 Scientific American, I reveal dramatic curves that show why the world will reach this temperature limit so quickly, and also why the recent slowdown in the rate of temperature increase, if it continues, will only buy us another 10 years. [ http://www.scientificamerican.com/artic ... d-by-2036/ ]
These numbers come from calculations made by me and several colleagues. We plugged values of Earth’s “equilibrium climate sensitivity”—a common measure of the heating effect of greenhouse gases—into a so-called energy balance model. Scientists use the model to investigate possible climate scenarios.
You can try this exercise yourself. The text below explains the variables and steps involved. You can download the climate data here and the model code here. And you can compare your results with mine, which are here. You can also change the variables to see what other future scenarios are possible. One note: the model runs on MatLab software, which can be obtained here.
We employed a simple zero-dimensional Energy Balance Model (“EBM”—see references 1 through 5 below) of the form:
[ http://www.scientificamerican.com/artic ... d-in-2036/ ]
REFERENCES
1. North, G. R., Cahalan, R. F. & Coakley, J. A., Energy balance climate models, Rev. Geophys. 19, 91–121 (1981).
2. Crowley, T. J. Causes of climate change over the past 1,000 years. Science 289, 270–277 (2000).
3. McGuffie, K. & Henderson-Sellers, A., A Climate Modeling Primer, 2nd Edition, Wiley, (1997).
4. Mann, M. E., Fuentes, J. D., Rutherford, S., Underestimation of Volcanic Cooling in Tree-Ring Based Reconstructions of Hemispheric Temperatures, Nature Geoscience, 5, 202–205 (2012).
5. Mann, M. E., Rutherford, S., Schurer, A., Tett, S.F.B., Fuentes, J. D., Discrepancies between the Modeled and Proxy-Reconstructed Response to Volcanic Forcing over the Past Millennium: Implications and Possible Mechanisms, J. Geophys. Res. 118, 7617-7627, doi:10.1002/jgrd.50609 (2013).
6. Wigley, T. M. L. & Raper, S. C. B., Natural variability of the climate system and detection of the greenhouse effect. Nature 344, 324–327 (1990).
7. IPCC, 2007: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change [S. Solomon, D. Qin, M. Manning, Z. Chen, M. Marquis, K. B. Averyt,
M.Tignor and H. L. Miller (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA.
8. Myhre, G., Highwood, E. J., Shine, K. P. & Stordal, F., New estimates of radiative forcing due to well mixed greenhouse gases, Geophys. Res. Lett. 25, 2715-2718, 1998.
9. Ammann, C. M. et al., Solar influence on climate during the past millennium: Results from transient simulations with the NCAR Climate System Model. Proc. Natl. Acad. Sci. 104, 3713–3718 (2007).