Radiative forcing of climate change

By J. Haigh. 2002

613 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/078e079c15af96ad0c11873d1996f8593272a955

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Citations in the corpus

Albedo Enhancement by Stratospheric Sulfur Injections: A Contribution to Resolve a Policy Dilemma? (2006, background): “Robock A (2008) 20 reasons why geoengineering may be a bad idea.”
Quantitative and qualitative evaluation of selected wheat varieties released since 1903 to increasing atmospheric carbon dioxide: can yield sensitivity to carbon dioxide be a factor in wheat performance? (2004, background): “It is anticipated that the global background [CO2] will continue to increase with concentrations projected to approach 500–700 mmol mol 1 by the end of the current century (Intergovernmental Panel on Climate Change scenario’s IS 92e and IS 92a, respectively, in Schimel et al., 1996).”
Aviation and global climate change in the 21st century (2009, methodology): “The approach taken to calculate aviation CO2 RF was to first calculate the CO2 concentrations attributable to aviation using a carbon-cycle model and then calculate its RF according to a simple function as recommended by the IPCC Third Assessment Report (Ramaswamy et al., 2001).”
How Much Warming are We Committed to and How Much can be Avoided? (2006, methodology): “It should be noted that mechanisms for the amplification of solar forcing are not yet well established (Ramaswamy et al., 2001, section 6.11.2; Stott et al., 2003).”
Bioenergy and sustainable development (2007, background): “9Nitrous oxide is a potent GHG with a global warming potential relative to carbon dioxide of 296 for a 100-year time horizon (122).”
Sensitivity studies of different aerosol indirect effects in mixed-phase clouds (2009, background): “The interactions of aerosols with clouds is the largest source of uncertainty for estimating the total anthropogenic forcing since pre-industrial times (Forster et al., 2007).”
Cumulative CO2 emissions: shifting international responsibilities for climate debt (2008, background): “Methane is the second largest contributor with 14% of CO2 equivalent emissions in 2000, but has a considerably shorter lifetime in the atmosphere, namely 10 years (Ramaswamy et al., 2001).”
Global Potential of Soil Carbon Sequestration to Mitigate the Greenhouse Effect (2003, background): “This imbalance is expressed in terms of “radiative forcing”, which is defined as the change in net irradiance (w/m2) at the tropopause after allowing the stratospheric temperatures to readjust to radiative equilibrium (Ramaswamy, 2001).”
The uncertainty about the social cost of carbon: A decomposition analysis using fund (2013, background): “ Leggett, J., W.J.Pepper, and R.J.Swart (1992), 'Emissions Scenarios for the IPCC: An Update', in Climate Change 1992 ‐ The Supplementary Report to the IPCC Scientific Assessment, 1 edn, vol. 1 J.T. Houghton, B.A. Callander, and S.K. Varney (eds.)”
Pelagic functional group modeling: Progress, challenges and prospects (2006, neutral): “Another impact on global climate associated with denitrification is production of N2O, which is an important greenhouse gas (its contribution to radiative forcing ranks behind only that of CO2 and methane; Ramaswamy et al., 2001).”
Estimating the social cost of non-CO2 GHG emissions: Methane and nitrous oxide (2012, background): “…of a given gas relative to a reference gas over a specified time horizon using the ratio of time integrated radiative forcing that results from the instantaneous release of one additional unit of a compound to that of one additional unit of a reference gas (commonly CO2) (Ramaswamy et al., 2001).”