Improved Attribution of Climate Forcing to Emissions
By D. Shindell, G. Faluvegi, D. Koch, Gavin A. Schmidt, N. Unger, S. Bauer. Science, 2009
884 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/2b0e4b548ef208f7690b48d9449bc0d54f8aad80
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- D. Shindell
- J. Hansen
- Gavin A. Schmidt
- D. Koch
- Makiko Sato
- Ronald L. Miller
- Svetlana Jevrejeva
- Aslak Grinsted
In Global and Planetary Change
- D. Shindell
- J. Hansen
- Gavin A. Schmidt
- D. Koch
- Makiko Sato
- G. Myhre
- Svetlana Jevrejeva
- John C. Moore
Citations in the corpus
- Cobenefits of climate and air pollution regulations The context of the European Commission Roadmap for moving to a low carbon economy in 2050 (2012, neutral): “(Hansen et al., 2000) therefore argued that the rapid warming in the past decades is largely due to non-CO2 GHGs. Shindell and co-workers argued that multi-gas climate mitigation strategies should account for the effect of short-lived air pollutants (Shindell et al., 2012; Shindell et al., 2009).”
- Configuration and assessment of the GISS ModelE2 contributions to the CMIP5 archive (2014, background): “…has chosen to focus on the importance of interactive atmospheric composition because of its importance in attributing emissions to climate change [Shindell et al., 2009], in responses to solar variability [Shindell et al., 2006a], and in the complex interactions between air pollution and climate…”
- Non-CO2 greenhouse gases and climate change (2011, background): “Reduced lOH • r would also mean longer lifetimes and enhanced climate influences for HFCs and hydrochlorofluorocarbons (HCFCs), decreased conversion of SO 2 to sulphate aerosol (less cooling) and changes in the cycling of tropospheric ozone, which is a powerful, very short-lived GH”
- The Marginal Damage Costs of Different Greenhouse Gases: An Application of FUND (2014, neutral): “2007), but not its effect on sulphate aerosols (Shindell et al. 2009).”
- Livestock and greenhouse gas emissions: The importance of getting the numbers right (2011, background): “The debate on how uch warming that CH4 causes is an ongoing one (Shindell et al., 2009).”
- Impacts of European livestock production: nitrogen, sulphur, phosphorus and greenhouse gas emissions, land-use, water eutrophication and biodiversity (2015, background): “Conversely, aerosols produced by NOx-driven photochemistry also affect climate, generally having a cooling effect (Simpson et al 2014, Shindell et al 2009).”
- Methane Leaks from North American Natural Gas Systems (2014, background): “Uncertainties about the role of CH4 in climate forcing (46) imply a need for reassessment of these decision points as knowledge improves.”
- Tropospheric ozone in CMIP6 simulations (2020, background): “Oxidant levels mediate the formation of secondary aerosols such as sulfate and nitrate and play a major role in the aerosol budget and burden with important consequences for radiative forcing (Shindell et al., 2009; Karset et al., 2018).”
- The social cost of atmospheric release (2015, methodology): “Radiative forcing due to short-lived species is based on a combination of modeling and literature analysis and includes indirect aerosol forcing [Shindell et al., 2012a; Shindell et al., 2009; United Nations Environment Programme and World Meteorological Organization, 2011].”
- Methane emissions from wetlands: biogeochemical, microbial, and modeling perspectives from local to global scales (2013, background): “One of the most exciting recent developments in this field is the attempt to integrate the different methodologies and spatial scales of biogeochemistry, molecular microbiology, and modeling, and thus this is a major focus of this review.”
- How will sea level respond to changes in natural and anthropogenic forcings by 2100? (2010, background): “Other unknowns include gas species interactions [Shindell et al., 2009] and uncertainty on feedback responses and climate sensitivity.”