Effect of aerosol on warm convective clouds: Aerosol‐cloud‐surface flux feedbacks in a new coupled large eddy model
By Hongli Jiang, G. Feingold. 2006
165 citations recorded by the source corpus.
Subfields: Atmospheric Science, Earth-Surface Processes, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/a86bb27d7097806334bd03fc349edff350c5a6ce
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Citations in the corpus
- Aerosol effects on clouds, precipitation, and the organization of shallow cumulus convection (2008, result): “2b; see also Jiang and Feingold (2006)].”
- Effects of aerosol optical properties on deep convective clouds and radiative forcing (2008, methodology): “Although the effects of aerosols including absorbing components on clouds and radiative forcing have been investigated by model simulations in previous studies [Johnson et al., 2004; Feingold et al., 2005; Jiang and Feingold, 2006; McFarquhar and Wang, 2006], few studies have simultaneously examin”
- Large-Eddy Simulations of Trade Wind Cumuli: Investigation of Aerosol Indirect Effects (2006, result): “Results in this study are generally consistent with Jiang and Feingold (2006), who simulated the effects of aerosol on cloud properties for warm continental cumulus with a different large-eddy simulation model coupled to a surface soil and vegetation model.”
- Can aerosol decrease cloud lifetime? (2009, background): “In recent years this hypothesis has come under scrutiny as high resolution models [Wang et al., 2003; Ackerman et al., 2004; Xue and Feingold, 2006; Jiang and Feingold, 2006] have revealed responses that are incongruent with this simple construct, and as observational evidence from satellite remote…”
- The Influence of Entrainment and Mixing Assumption on Aerosol–Cloud Interactions in Marine Stratocumulus (2009, background): “This evaporation– entrainment effect has been termed an evaporation– entrainment feedback in studies of cumulus clouds (Xue and Feingold 2006; Jiang and Feingold 2006).”
- Aerosol effects on the lifetime of shallow cumulus (2006, background): “1 mm d; (ii) A continental convective case from the Smoke, Aerosols, Clouds, Rainfall, and Climate (SMOCC) experiment as simulated in Jiang and Feingold (2006). This surface-forced case generates somewhat deeper clouds ranging from a few 100 m to 3 km and CF of ~ 20%.”
- Developments in the CSU-RAMS Aerosol Model: Emissions, Nucleation, Regeneration, Deposition, and Radiation (2013, unknown): “The RAMS model has proven to be versatile across atmospheric scales as a large-eddy-simulation model (e.g., Jiang et al. 2001; Jiang and Feingold 2006), cloudresolving model (e.”