Indirect effect of sulfate and carbonaceous aerosols: A mechanistic treatment

By Ulrike Lohmann, Johann Feichter, J. Penner, R. Leaitch. 2000

225 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/c285ebee89bc006b909e58e1940fac893be96554

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Citations in the corpus

Total aerosol effect: radiative forcing or radiative flux perturbation? (2009, background): “1 Cloud albedo and cloud lifetime effect Lohmann and Feichter(1997), Rotstayn(1999), Lohmann et al. (2000), Jones et al.(2001), Williams et al. (2001), Ghan et al.(2001), Lohmann and Lesins(2002), Menon et al. (2002), Kristjánsson(2002), Peng and Lohmann(2003), Kristjánsson et al.(2005), Ming et…”
Radiative forcing of climate change (2002, background): “The indirect aerosol forcing is also sensitive to the treatment of the pre-industrial aerosol concentration and properties (Jones et al., 1999; Lohmann et al., 2000) which remain poorly characterised, the representation of the microphysics of mid-level clouds (Lohmann et al.”
A study of internal and external mixing scenarios and its effect on aerosol optical properties and direct radiative forcing (2002, background): “, 1995; Jacobson, 2001b] and for the indirect effect, where the anthropogenic aerosols affect the radiative properties of clouds [Chuang et al., 1997; Lohmann et al., 2000]).”
Possible Aerosol Effects on Ice Clouds via Contact Nucleation (2002, background): “However, the parameterization of heterogeneous freezing that is used in Lohmann et al. (2000) depends on cloud droplet size and number, and thus could have been affected by changes in aerosol load.”
Aerosol–climate interactions in the Norwegian Earth System Model – NorESM1-M (2012, background): “Lohmann et al. (2000) showed that a reduction of the minimum cloud droplet number concentration (CDNC) from 40 to 10 cm−3 led to a 70 % increase in the joint first and second indirect effect.”
A New Two-Moment Bulk Stratiform Cloud Microphysics Scheme in the Community Atmosphere Model, Version 3 (CAM3). Part II: Single-Column and Global Results (2008, methodology): “58 is used (Lohmann et al. 2000), where Na is the number (cm (3)) and mSO4 is the mass of sulfate ( g m (3)).”
Constraining cloud droplet number concentration in GCMs suppresses the aerosol indirect effect (2009, methodology): “Our systematic investigations show a similar reduction to the results by Lohmann et al. [2000] with ECHAM4 and by Wang and Penner [2009] with IMPACT-CAM for the cloud albedo effect only (Figure 2b).”
Limits to the Aerosol Indirect Radiative Effect Derived from Observations of Ship Tracks (2002, background): “8 Wm (Lohmann and Feichter 1997, Rotstayn 1999, Lohmann et al. 2000). About half the enhancement in the simulations is due to changes in cloud albedos, when the cloud liquid water is kept constant, and half is due to changes in cloud liquid water and cloud fraction in response to changes in precipit”
Aerosol cloud precipitation interactions. Part 1. The nature and sources of cloud-active aerosols (2008, background): “…tended to assume that the conversion of hydrophobic soot to hydrophilic particles had exponential lifetimes of some 35–80 h (Cooke and Wilson, 1996; Lohmann et al., 2000; Wilson et al., 2001), but recent studies (Riemer et al., 2004; Johnson et al., 2005b) suggest that conversion can occur as…”
Efficacy of climate forcings (2005, background): “Shine [2005] also concludes thatMinnis et al. [2004] overestimate the effect of contrails for this reason.”
Single‐particle measurements of midlatitude black carbon and light‐scattering aerosols from the boundary layer to the lower stratosphere (2006, background): “BCA also contributes to indirect forcing of climate by acting as cloud condensation nuclei [ Lohmann et al., 2000; Twohy and Poellot, 2005].”
Cloud susceptibility and the first aerosol indirect forcing: Sensitivity to black carbon and aerosol concentrations (2002, background): “The increased cloud longevity could give rise to a higher cloud cover fraction and liquid water content and further enhance the cooling [Lohmann and Feichter, 1997; Rotstayn, 1999; Lohmann et al., 2000].”