Global Climate Change: Past and Future
`The balance of evidence suggests that there is a discernible human influence on global climate ' Intergovernmental Panel on Climate Change (United Nations), Second Assessment Report, 1996
`There is new and stronger evidence that most of the warming observed over the last 50 years is attributable to human activity' Intergovernmental Panel on Climate Change (United Nations), Third Assessment Report, 2001
`Most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations’ Intergovernmental Panel on Climate Change (United Nations), Fourth Assessment Report, 2007
OBSERVATIONS
Surface Temperature Changes Boxes: back to mid 19 th century Gray: back to beginning of 20th century
Surface Temperature Changes
Internally Consistent Changes in Other Variables
Greenhouse Gases and Warming CO 2 Related?
ENHANCED GREENHOUSE EFFECT?
TREE RINGS
CORALS
ICE CORES
VARVED LAKE SEDIMENTS
HISTORICAL DOCUMENTS
RECONSTRUCTED GLOBAL TEMPERATURE PATTERNS
Reconstructed Surface Temperatures Climate Change 2001: The Scientific Basis, Houghton, J.T., et al. (eds.), Cambridge Univ. Press, Cambridge, 2001
Reconstructions of Northern Hemisphere mean temperatures for the last 1000 years and instrumental record (black line) From “Wikipedia”
Mt Kilimanjaro
Thompson, L. G., Mosley-Thompson, E., Davis, M. E., Lin, P. N., Henderson, K., and Mashiotta, T. A., 2003, Tropical glacier and ice core evidence of climate change on annual to millennial time scales, Climatic Change, v. 59, p
MODEL SIMULATIONS
The climate represents a coupled system consisting of an atmosphere, hydrosphere, biosphere, and cryosphere
General Circulation Models (GCMs) take into account the full three-dimensional structure of the atmosphere and ocean
Natural Volcanism Solar CLIMATE FORCINGS Crowley, T.J., Causes of Climate Change Over the Past 1000 Years, Science, , 2000.
CLIMATE FORCINGS Anthropogenic Greenhouse Gases Industrial Aerosols Climate Change 2001: The Scientific Basis, Houghton, J.T., et al. (eds.), Cambridge Univ. Press, Cambridge, 2001
Simulated Annual Global Mean Surface Temperatures Climate Change 2001: The Scientific Basis, Houghton, J.T., et al. (eds.), Cambridge Univ. Press, Cambridge, 2001 Forced Model simulations
Simulated Annual Global Mean Surface Temperatures Climate Change 2001: The Scientific Basis, Houghton, J.T., et al. (eds.), Cambridge Univ. Press, Cambridge, 2001 Forced Model simulations
Simulated Annual Global Mean Surface Temperatures Climate Change 2001: The Scientific Basis, Houghton, J.T., et al. (eds.), Cambridge Univ. Press, Cambridge, 2001 Forced Model simulations
Jones, P.D., Mann, M.E., Climate Over Past Millennia, Reviews of Geophysics, 42, RG2002, doi: /2003RG000143, 2004.
Climate Change 2001: The Scientific Basis, Houghton, J.T., et al. (eds.), Cambridge Univ. Press, Cambridge, 2001 Future Surface Temperatures Trends?
Model Predictions Climate Change 2001: The Scientific Basis, Houghton, J.T., et al. (eds.), Cambridge Univ. Press, Cambridge, 2001
Model Predictions
Possible Impacts? Warmer summer temperatures +less/no increase in continental precipitation = more frequent summer drought
Greenland Melting… (source: Arctic Impacts of Arctic Warming, Cambridge Press, 2004). Possible Impacts?
…Sea Level Rise
Possible Impacts? …Sea Level Rise +10 meters
Possible Impacts? …More Destructive Hurricanes Katrina (Aug ’05)
Possible Impacts? …More Destructive Hurricanes Rita (Sep ’05)
Possible Impacts? …More Destructive Hurricanes Wilma (Oct ’05)
Climate Model Predictions Knutson, T. K., and R. E. Tuleya, 2004: Impact of CO2-induced warming on simulated hurricane intensity and precipitation: Sensitivity to the choice of climate model and convective parameterization. Journal of Climate, 17(18),
Emanuel, K. (2005), Increasing destructiveness of tropical cyclones over the past 30 years, Nature, online publication; published online 31 July 2005 | doi: /nature03906 Hurricane Statistics
CONCLUSIONS Recent global surface temperatures are unprecedented in a long-term context It is difficult to explain the recent surface warming in terms of natural climate variability Recent surface warming is largely consistent with simulations of the effects of anthropogenic influence on climate Possible impacts of anthropogenic climate change this century include increased drought, coastal flooding, and more destructive Atlantic Hurricanes
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