Satellite-based estimate of the direct and indirect aerosol climate forcing
By Johannes Quaas, O. Boucher, N. Bellouin, S. Kinne. 2008
337 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/81c1eee80dcf837d0bd12adcf557ad6790a49f18
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
- Hugh Morrison
- Andrew Gettelman
- Steven Ghan
- Xiaohong Liu
- C. Hoose
- J. Kristjánsson
- Minghuai Wang
- J. Penner
In Global and Planetary Change
- Hugh Morrison
- Andrew Gettelman
- Steven Ghan
- Xiaohong Liu
- C. Hoose
- J. Kristjánsson
- Minghuai Wang
- J. Penner
Citations in the corpus
- Next-generation angular distribution models for top-of-atmosphere radiative flux calculation from CERES instruments: validation (2015, methodology): “Next, a fit from 15 Rahman et al. (1993) is used to account for the albedo dependence on solar zenith angle in each μ0 interval.”
- The Distribution of Cloud Horizontal Sizes (2011, background): “A number of observational studies used to estimate aerosol indirect effects rely on correlations between cloud microphysical properties and aerosol properties derived from neighboring clear-sky regions (e.g., Quaas et al. 2008).”
- Constraining cloud droplet number concentration in GCMs suppresses the aerosol indirect effect (2009, result): “[19] These results leave the modeling community with the dilemma that large magnitude negative aerosol indirect effects (lower than about 1.2 W m 2) are not in agreement with inverse calculations [Hegerl et al., 2007] and satellite estimates [e. g., Quaas et al., 2008].”
- Bounding Global Aerosol Radiative Forcing of Climate Change (2020, methodology): “The1120 intrinsic/extrinsic methodology closely agrees with earlier methods (e.g Quaas et al., 2008),1121 as shown by Amiri-Farahani et al. (2017) and Christensen et al. (2017).1122 8.1 Adjustments in liquid water path L1123 The sensitivity of L to Nd varies regionally (Han et al., 2002) and is…”
- Constraining the aerosol influence on cloud liquid water path (2018, methodology): “Such observed relationships have been used to estimate the instantaneous radiative forcing (RFaci) from a change in Nd (e.g. Quaas et al., 2008; Stevens et al., 2017; McCoy et al., Published by Copernicus Publications on behalf of the European Geosciences Union.”
- Satellite-based estimate of global aerosol-cloud radiative forcing by marine warm clouds (2014, background): “1 Wm over ocean (satellite-based estimation; Quaas et al., 2008).”
- Constraining cloud lifetime effects of aerosols using A‐Train satellite observations (2012, methodology): “Satellite observations have been used to constrain cloud albedo effects in climate models and typically produce smaller aerosol indirect forcing than solely model-based estimates [e.g., Lohmann and Lesins, 2002; Quaas and Boucher, 2005; Quaas et al., 2008].”