Indirect Aerosol Forcing, Quasi Forcing, and Climate Response

By Leon D. Rotstayn, J. Penner. 2001

140 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/a69bbfdded970c35f8edbfe24370c78b6e46cea1

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

1. Hugh Morrison
2. Andrew Gettelman
3. C. Hoose
4. Ulrike Lohmann
5. Steven Ghan
6. P. Stier
7. J. Kristjánsson
8. Johannes Quaas

In Global and Planetary Change

1. Hugh Morrison
2. Andrew Gettelman
3. Ulrike Lohmann
4. C. Hoose
5. Steven Ghan
6. P. Stier
7. J. Kristjánsson
8. Johannes Quaas

Citations in the corpus

• Aerosol indirect effects – general circulation model intercomparison and evaluation with satellite data (2009, background): “The short-wave total aerosol effect (all effects combined) is diagnosed as a radiative flux perturbation or fixed-SST forcing (Rotstayn and Penner, 2001; Shine et al., 2003; Quaas et al., 2009), where in the case of the nudged simulations the tropospheric pro-files also were kept fixed by construction.”
• A comparison of climate response to different radiative forcings in three general circulation models: towards an improved metric of climate change (2003, background): “More recent work examining the concept can be found in Hansen et al. (1997), Christiansen (1999), Forster et al. (2000), Rotstayn and Penner (2001) and Stuber et al. (2001a, b). The overall conclusion of these works is that, compared to the uncertainties in the actual value of k in any one model, ”
• Total aerosol effect: radiative forcing or radiative flux perturbation? (2009, methodology): “…Lohmann and Feichter(1997), Rotstayn(1999), Lohmann et al.(2000), Kiehl et al.(2000), Jones et al.(2001), Williams et al.(2001), Ghan et al.(2001), Rotstayn and Penner(2001), Chuang et al.(2002), Kristjánsson(2002), Rotstayn and Liu (2003), Suzuki et al.(2004), Quaas et al.(2004), Dufresne et…”
• Anthropogenic and Natural Radiative Forcing (2014, unknown): “…to aerosol-induced changes in clouds (e.g., effects previously denoted as cloud lifetime or semi-direct effects; see Figure 7.3) that are not amenable to characterization by RF (e.g., Rotstayn and Penner, 2001; Shine et al., 2003; Hansen et al., 2005; Lohmann et al., 2010; Ban-Weiss et al., 2012).”
• An alternative to radiative forcing for estimating the relative importance of climate change mechanisms (2003, methodology): “…have indicated that in any one model, l is approximately constant whether Fa is caused by, for example, changes in greenhouse gas concentrations, solar output or scattering aerosols [e.g., Boer and Yu, 2003; Hansen et al., 1997; IPCC, 1995; Joshi et al., 2003; Rotstayn and Penner, 2001].”
• Global indirect aerosol effects: a review (2004, unknown): “For instance, Rotstayn and Penner (2001) showed that the combined Twomey and cloud lifetime effect is smaller than the sum of the individual effects (Table 2).”
• A New Double-Moment Microphysics Parameterization for Application in Cloud and Climate Models. Part I: Description (2005, background): “Most studies have focused on aerosol modification of the droplet population (e.g., Albrecht 1989; Coakley and Walsh 2002; Ghan et al. 2001; Penner and Rotstayn 2001; Feingold et al. 2003), but aerosol–ice interactions may also have a significant influence on ice and mixedphase clouds (DeMott et al”
• Mesoscale modeling of springtime Arctic mixed-phase stratiform clouds using a new two-moment bulk microphysics scheme (2005, background): “Most studies have focused on aerosol modification of the droplet population (e.g., Albrecht 1989; Coakley and Walsh 2002; Ghan et al. 2001; Rotstayn and Penner 2001; Feingold et al. 2003), but aerosol–ice interactions may also have a significant impact on ice- and mixed-phase clouds (e.”
• Cloud susceptibility and the first aerosol indirect forcing: Sensitivity to black carbon and aerosol concentrations (2002, unknown): “Thus, the forcing can be calculated exactly, keeping these quantities fixed and calling the radiation subroutines of the model twice [Rotstayn and Penner, 2001].”
• Technical Note: Estimating aerosol effects on cloud radiative forcing (2013, background): “, 2012) by the change in the cloud radiative forcing when anthropogenic emissions are introduced in simulations: 1C, where1 is the difference between atmosphere simulations with and without anthropogenic emissions but the same ocean conditions (Rotstayn and Penner, 2001; Haywood et al., 2009) and na”
• Extratropical Cooling, Interhemispheric Thermal Gradients, and Tropical Climate Change (2012, background): “AGCM simulations by Rotstayn et al. (2000), followed by Rotstayn & Penner (2001) and Williams et al. (2001), were the first to show that the global climate impacts from late-twentieth-century anthropogenic aerosol distributions cause NH-wide cooling, leading to an interhemispheric thermal gradient,…”
• The Radiative Forcing Model Intercomparison Project (RFMIP): Experimental Protocol for CMIP6 (in open review: 10.5194/gmd-2016-88) (2016, background): “…from temporal variations in N and 1T following abruptly applied changes in composition (Gregory et al., 2004), or by approximately suppressing 1T by fixing sea surface temperatures (SSTs) and inferring effective radiative forcing from N following Hansen et al. (2005) and Rotstayn and Penner (2001).”