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Climate Change Detection / Attribution. Organizer: Martin Visbeck, Columbia University. Co-organizer/Chair: Michael E. Mann, University of Virginia. SPEAKERS: Gabi Hegerl, Duke University Drew Shindell, NASA-Goddard Institute for Space Studies. National Academy of Sciences
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Climate Change Detection / Attribution Organizer: Martin Visbeck, Columbia University Co-organizer/Chair: Michael E. Mann, University of Virginia SPEAKERS: Gabi Hegerl, Duke University Drew Shindell, NASA-Goddard Institute for Space Studies National Academy of Sciences Thirteenth Annual Symposium on Frontiers of Science November 8-10, 2001
Climate Change Detection / Attribution Introduction (Mann) 25 minQ&A 5 minUse of Models in Detection/Attribution (Hegerl) 25 minQ&A 5 minCauses of N.Hemisphere winter warming (Shindell) 25 minQ&A 5 minDiscussion 30 min National Academy of Sciences Thirteenth Annual Symposium on Frontiers of Science November 8-10, 2001
Introduction to the Problem of Climate Change Detection and Attribution Michael E. Mann Department of Environmental Sciences University of Virginia National Academy of Sciences Thirteenth Annual Symposium on Frontiers of Science November 8-10, 2001
`There is new and stronger evidence that most of the warming observed overthe last 50 years is attributable to human activity' Intergovernmental Panel on Climate Change (United Nations), Third Assessment Report, 2001
OVERVIEW • The Empirical Record • Model Predictions • Comparison between the two • Key Outstanding issues
THE EMPIRICAL RECORD Surface Temperature Changes
Climate Change 2001: The Scientific Basis, Houghton, J.T., et al. (eds.), Cambridge Univ. Press, Cambridge, 2001
INSTRUMENTAL TEMPERATURE RECORD GLOBAL PROXY CLIMATE RECORDS
Greenhouse Gases and Warming CO2 Related?
SIMULATED ANNUAL MEAN TREND 1949-1997 Knutson, T.R., T.L. Delworth, K.W. Dixon, and R.J. Stouffer, Model assessment of regional surface temperature trends (1949-1997), Journal of Geophysical Research, 104, 30981-30996, 1999.
Observations Modeled Natural Variability
OBSERVED ANNUAL MEAN TREND 1949-1997 Knutson, T.R., T.L. Delworth, K.W. Dixon, and R.J. Stouffer, Model assessment of regional surface temperature trends (1949-1997), Journal of Geophysical Research, 104, 30981-30996, 1999.
SIMULATED ANNUAL MEAN TREND 1949-1997 Knutson, T.R., T.L. Delworth, K.W. Dixon, and R.J. Stouffer, Model assessment of regional surface temperature trends (1949-1997), Journal of Geophysical Research, 104, 30981-30996, 1999.
Inconsistent with Natural Variability Inconsistent with Greenhouse+ Sulphate Forcing
Greenhouse vs. Solar Vertical Fingerprint ECHAM3/LSG MODEL Climate Change 2001: The Scientific Basis, Houghton, J.T., et al. (eds.), Cambridge Univ. Press, Cambridge, 2001
CLIMATE FORCINGS Anthropogenic Industrial Aerosols Greenhouse Gases
1000 1200 1400 1600 1800 2000 CLIMATE FORCINGS Volcanism Solar Natural
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
Science Energy Balance Model (“EBM”) simulation
Future Surface Temperatures Trends Climate Change 2001: The Scientific Basis, Houghton, J.T., et al. (eds.), Cambridge Univ. Press, Cambridge, 2001
EL NINO/SOUTHERN OSCILLATION (“ENSO”) Substantial interannual climate variability associated with ENSO, but decadal variability is also evident as well. The recent decadal trend towards El Nino conditions could be natural or anthropogenic. Multivariate ENSO Index (“MEI”)
NORTH ATLANTIC OSCILLATION Negative Phase Positive Phase
NORTH ATLANTIC OSCILLATION Trend in NAO in past couple decades explains enhanced recent warming in certain regions of Northern Hemisphere
Shindell et al (Science, in press) Empirical LIA winter cooling in Europe associated with an NAO trend due to solar irradiance changes, interacting w/ stratospheric atmospheric dynamics and chemistry NASA/GISS Model
NORTH ATLANTIC OSCILLATION This NAO trend could be Anthropogenic
CONCLUSIONS • Recent global surface temperatures are unprecedented this century, and likely at least the past millennium • 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 • Unresolved issues regarding the precise sensitivity of the climate to forcing, and changes in ENSO, NAO, and regional responses