| Citation | Authors' Organization | Pub. Date | Cited by... | Findings on anthropogenic forcing [causes] | |||
| Finds Anthro. Causes | Recognizes Anthro. Causes | Finds no Anthro. Causes | NA or Other | ||||
| Responsibility for Past and Future Global Warming: Uncertainties in Attributing Anthropogenic Climate Change - ►unfccc.int [PDF] Michel Den Elzen, Michiel Schaeffer Climatic Change, Volume 54, Numbers 1-2, July 2002 | Dutch National Institute for Public Health and the Environment, Bilthoven, The Netherlands Royal Dutch Meteorological Institute (KNMI), De Bilt, The Netherlands | 2002 | 32 | X | X | ||
| Optimal choice of climate change policy in the presence of uncertainty William A. Pizer Resource and Energy Economics, Elsevier, Volume 21, Pages 255-287, 304 August 1999 | Resources for the Future, Washington DC [This organization describes itself as a nonprofit and nonpartisan think tank] | 1999 | 95 | X | |||
| Predicting the impacts of climate change on the distribution of species: are bioclimate envelope models useful? - ►gbif.org [PDF] Richard G. Pearson, Terence P. Dawson Global Ecology and Biogeography, Volume 12 Issue 5, Pages 361-371, 21 Aug 2003 | Environmental Change Institute, School of Geography and the Environment, University of Oxford, Oxford, UK | 2003 | 305 | X | |||
| [CITATION] On multi-fingerprint detection and attribution of greenhouse gas- and aerosol forced climate change Gabriele C. Hegerl, K. Hasselmann, U. Cubasch, J.F.B. Mitchell, E. Roeckner, R. Voss, J. Waszkewitz Climate Dynamics, Volume. 13,Issue 9, pp. 613-634, 1997 | Max Planck Institut für Meteorologie, Hamburg, Germany Deutsches Klimarechenzentrum, Hamburg, Germany Hadley Centre for Climate Prediction and Research, Meteorological Office, Bracknell, Berkshire UK | 1997 | 48 | X | |||
| Excerpted from abstract for the reference above: "...are found to represent a significant climate change at the 97.5% confidence level ... we consider our results sufficiently robust to have some confidence in our finding that the observed climate change is consistent with a combined greenhouse gas and aerosol forcing..." | |||||||
| [BOOK] Climate Change 1994: Radiative Forcing of Climate Change and an Evaluation of the IPCC IS92 Emission Scenarios A Report of Working Group 1 of the Intergovernmental Panel on Climate Change J.T. Houghton et al(editors) Cambridge University Press, 1994 | IPCC: Many editors, authors, and organizations | 1994 | 247 | X | |||
| [HTML] ►Changes in sea level Included in Climate Change 2001: The Scientific Basis, IPCC JA Church, JM Gregory, P Huybrechts, M Kuhn, K Lambeck, MT Nhuan, D Qin, PL Woodworth Cambridge University Press, 2001 | IPCC: Many editors, authors, and organizations | 2001 | 338 | X | |||
| Early effects of climate change: do they include changes in vector-borne disease? RS Kovats, DH Campbell-Lendrum, AJ McMichael, A Woodward, JS Cox | Department of Epidemiology and Population Health, London School of Hygiene and Tropical Medicine, London, UK | 2001 | 97 | X | X | ||
| Climate response to increasing levels of greenhouse gases and sulphate aerosols J.F.B. Mitchell, T.C. Johns, J.M. Gregory, S.F.B. Tett Nature Vol. 376, pp. 501-504, 10 August 1995 | Hadley Centre for Climate Prediction and Researche, Meteorological Office, Bracknell, UK | 1995 | 472 | X | |||
| Seminal
paper, or possibly corroboration of a seminal paper: This shows that
match of model results with observations is much better when the models
account for suflfate aerosols than when accounting for only greenhouse
gases. Excerpt from end of abstract of reference above: "We predict a future global mean warming of 0.3 K per decade for greenhouse gases alone, or 0.2 K per decade with sulphate aerosol forcing included. By 2050, all land areas have warmed in our simulations, despite strong negative radiative forcing in some regions." | |||||||
| External Control of 20th Century Temperature by Natural and Anthropogenic Forcings - ►sfsu.edu [PDF] Peter A. Stott, S.F.B. Tett, G.S. Jones, M.R. Allen, J.F.B. Mitchell, G.J. Jenkins | Meteorological Office, Hadley Centre for Climate Prediction and Researche, Bracknell, UK Space Science and Technology Department, Rutherford Appleton Laboratory, Didcot, Oxfordshire, UK Department of Physics, University of Oxford, Oxford, UK | 2001 | 246 | X | |||
| Excerpt from abstract of reference above: "... both natural and anthropogenic factors have contributed significantly to 20th century temperature changes." | |||||||
| Forcings and chaos in interannual to decadal climate change J. Hansen et al, in total 43 co-authors Journal of Geophysical Research, Vol. 102 no. 25, | Many organizations | 1997 | 87 | X | |||
| Excerpt from abstract: "Both a natural radiative forcing (volcanic aerosols) and an anthropogenic forcing (ozone depletion) leave clear signatures in the simulated climate change that are identified in observations. ... One implication of the disequilibrium forcing is an expectation of new record global temperatures in the next few years." [Subsequent observations confirmed this prediction.] | |||||||