Climate response to regional radiative forcing during the twentieth century
By D. Shindell, G. Faluvegi. 2009
684 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/404561fb5ac7784ee00ed9b990aa2a79abf3b497
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
- Xiaohong Liu
- Steven Ghan
- R. Easter
- Ulrike Lohmann
- D. Shindell
- G. Myhre
- Michael Schulz
- Johannes Quaas
In Global and Planetary Change
Citations in the corpus
- Black soot and the survival of Tibetan glaciers (2009, background): “These studies (14, 18, 19, 25) suggest that black soot is responsible for a substantial fraction of the regional warming of the past century, comparable to the fraction attributable to carbon dioxide.”
- Climate, Health, Agricultural and Economic Impacts of Tighter Vehicle-Emission Standards (2011, methodology): “Global and regional climate responses are calculated using simple energy-balance equations derived from coupled ocean–atmosphere model”
- Radiative forcing in the ACCMIP historical and future climate simulations (2013, background): “…on observed temperature changes, ocean heat uptake, and cacluated non-aerosol forcings produce ERF best estimates of−0.8 to−1.6 W m−2 (Murphy et al., 2009; Shindell and Faluvegi, 2009; Church et al., 2011; Hansen et al., 2011), though some find smaller values (e.g. Libardoni and Forest, 2011).”
- Total aerosol effect: radiative forcing or radiative flux perturbation? (2009, background): “5 Inverse estimates of the direct and indirect aerosol effects Andronova and Schlesinger(2001), Knutti et al.(2002), Gregory et al.(2002), Forest et al.(2002), Knutti et al. (2003), Forest et al.(2006), Stott et al.(2006), Shindell and Faluvegi (2009), Murphy et al.(2009) Acknowledgements.”
- Anthropogenic and Natural Radiative Forcing (2014, background): “For example, forcings over Northern Hemisphere (NH) middle and high latitudes induce snow and ice albedo feedbacks more than forcings at lower latitudes or in the Southern Hemisphere (SH) (e.g., Shindell and Faluvegi, 2009).”