Global warming in the twenty-first century: an alternative scenario.
By J. Hansen, M. Sato, R. Ruedy, Andrew A. Lacis, V. Oinas. Proceedings of the National Academy of Sciences of the United States of America, 2000
1,095 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/25103817e1a193f2a605513ffd0d370987d85eff
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Citations in the corpus
- Wavelength Dependence of the Absorption of Black Carbon Particles: Predictions and Results from the TARFOX Experiment and Implications for the Aerosol Single Scattering Albedo (2002, background): “Black carbon particles have received increased interest recently since Hansen et al. (2000) indicate that it is perhaps more cost effective to control black carbon particles than CO2 at the present time.”
- Cobenefits of climate and air pollution regulations The context of the European Commission Roadmap for moving to a low carbon economy in 2050 (2012, positive): “The effect of fossil fuel combustion on the radiative forcing is actually limited at relatively short timescales (decades) through the offsetting effects of CO2 and aerosol emissions at these timescales (Hansen et al., 2000; Wigley, 1991).”
- Issues related to mitigation in the long-term context (2007, background): “In addition, airborne black carbon absorbs solar radiation and thus contributes to the warming of the climate (Hansen et al. 2000; Andrae 2001; Jacobson 2001).”
- Anaerobic Metabolism: Linkages to Trace Gases and Aerobic Processes (2003, background): “These characteristics have inspired the recommendation that efforts to slow the pace of global warming should focus initially on abating CH4 emissions (Hansen et al., 2000; Fuglestvedt et al., 2000).”
- Evaluating Ultraviolet Radiation Exposure with Satellite Data at Sites of Amphibian Declines in Central and South America (2001, background): “The pervasive and global extent of pollution plumes, especially particulates (e.g., soot), was recently implicated in climate changes ( Hansen et al. 2000).”
- Dangerous human-made interference with climate: a GISS modelE study (2006, methodology): “(a) Greenhouse gas amounts, (b) growth rates, and(c) resulting forcings and(d) forcing growth rates for IPCC (2001), “alternative”, and “2C” scenarios (Hansen et al., 2000; Hansen and Sato, 2004).”
- Black carbon vertical profiles strongly affect its radiative forcing uncertainty (2012, background): “Sciences cc ss pen This warming effect of BC has led to suggestions, both in the scientific community (Editorial Nature, 2009; Grieshop et al., 2009; Shindell et al., 2012; Hansen et al., 2000) and among policy makers, for reduction of BC emissions to mitigate global warming.”
- Earth's energy imbalance and implications (2011, background): “An equation for climate forcing as a function of CO 2 amount is given in Table 1 of Hansen et al. (2000). basic quantum physics and verified by laboratory measurements to an accuracy of a few percent.”
- Efficacy of climate forcings (2005, background): “Besides CO2, methane and soot are potentially the largest global anthropogenic forcings, although estimates of the soot forcing have varied widely [Ramaswamy et al., 2001; Hansen et al., 2000; Jacobson, 2001; Penner, 2001; Penner et al., 2003].”
- Paleoclimate Implications for Human-Made Climate Change (2011, methodology): “Figure 6 shows that average temperature in the early Pliocene, when sea level was of the order of 20 m higher than today, was about 1 C above peak Holocene temperature.”