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Global Environmental Change: Technology and the Future of Planet Earth Where will all the heat go?. Eugene S. Takle Agronomy Department Geological and Atmospheric Science Department Iowa State University Ames, Iowa 50011 gstakle@iastate.edu. Mechanical Engineering 484X, 8 February 2005.
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Global Environmental Change:Technology and the Future of Planet EarthWhere will all the heat go? Eugene S. Takle Agronomy Department Geological and Atmospheric Science Department Iowa State University Ames, Iowa 50011 gstakle@iastate.edu Mechanical Engineering 484X, 8 February 2005
Outline • Evidence for global climate change • Future atmospheric carbon dioxide concentrations • Simulations of global climate and future climate change • How much change is “safe”? • Summary
2040 Carbon Dioxide and Temperature 2005
Carbon Dioxide and Temperature Stabilization at 550 ppm
Carbon Dioxide and Temperature “Business as Usual” (fossil intensive) 2100
Associated Climate Changes • Global sea-level has increased 1-2 mm/yr • Duration of ice cover of rivers and lakes decreased by 2 weeks in N. Hemisphere • Arctic ice has thinned substantially, decreased in extent by 10-15% • Reduced permafrost in polar, sub-polar, mountainous regions • Growing season lengthened by 1-4 days in N. Hemisphere • Retreat of continental glaciers on all continents • Poleward shift of animal and plant ranges • Snow cover decreased by 10% • Earlier flowering dates • Coral reef bleaching Source: Intergovernmental Panel on Climate Change, 2001 Report
Mann, M. E., R. S. Bailey, and M. K. Hughes, 1999: Geophysical Research Letters 26, 759.
El Chichon (1982) Agung, 1963 Mt. Pinatubo (1991) Hansen, Scientific American, March 2004
Source: IPCC, 2001: Climate Change 2001: The Scientific Basis
Source: IPCC, 2001: Climate Change 2001: The Scientific Basis
Change in Downwelling Longwave Radiation vs. Change in Surface Temperature Normalized Change Longwave Down Surface (2m) Temperature From GEWEX News, 14, 1 (November 2004); http://gewx.org/gewex_nwsltr.html
NASA photographs show the minimm Arctic sea ice concentration in 1979 at left and in 2003.Satellite passive microwave data since 1970s indicate a 3% decrease per decade in arctic sea ice extent.
Since 1979, the size of the summer polar ice cap has shrunk more than 20 percent. (Illustration from NASA) (http://www.nrdc.org/globalWarming/qthinice.asp)
Source: Jerry Meehl, National Center for Atmospheric Research
The planet is committed to a warming over the next 50 years regardless of political decisions Source: National Center for Atmospheric Research
Source: Intergovernmental Panel on Climate Change, 2001 Report
40% Probability 5% Probability Source: Intergovernmental Panel on Climate Change, 2001 Report
Climate Change Projected for 2100 Rapid Economic Growth Slower Economic Growth
Source: Corell, R. W., 2004: Impacts of a warming Arctic. Arctic Climate Impact Assessment (www.acia.uaf.edu) Cambridge University Press (www.cambridge.org).
Kennedy Space Center Impact of a 1-m rise in sea level on low-lying areas Areas subjected to Inundation with a 1 m (~3 ft) rise in sea level Miami Source: Corell, R. W., 2004: Impacts of a warming Arctic. Arctic Climate Impact Assessment (www.acia.uaf.edu) Cambridge University Press (www.cambridge.org).
Climate Surprises • Breakdown of the ocean thermohaline circulation (Greenland melt water) • Breakoff of the West Antarctic Ice Sheet
Kennedy Space Center Areas subjected to Inundation with a 1 m (~3 ft) rise in sea level Miami
Heat Absorption by Ice Masses • Arctic ice • Antarctic ice • Mountain glaciers • Mt. Kilimanjaro glacier will disappear within 20 years • Chacaltaya glacier, Andes Mountains, will disappear in 7-8 years (water supply for La Paz, Bolivia) • Italian Alps will lose its permanent ice in 20-30 years • Glacier National Park is losing ice at an accelerating rate
What Consitutes “Dangerous Anthropogenic Interference with the Climate System”? James Hansen, Director of the NASA Goddard Institute for Space Studies: * Radiative forcing limit: 1 Watt/ m2 * 1 oC additional rise in global mean temperature
Summary • Climate change is real and we need to be doing something about it • The longer we wait, the fewer our options • Regional patterns of warming will be complicated • Climate surprises can’t be discounted • We need dialog on what constitutes “dangerous anthropogenic interference with the climate system”
For More Information • For peer-reviewed evidence supporting everything you have seen in this presentation, see my online Global Change course: http://www.meteor.iastate.edu/gccourse • Contact me directly: gstakle@iastate.edu • For a copy of this presentation: http://www.meteor.iastate.edu/faculty/takle/