Large-Eddy Simulations of Trade Wind Cumuli: Investigation of Aerosol Indirect Effects

By H. Xue, G. Feingold. 2006

308 citations recorded by the source corpus.

Subfields: Atmospheric Science, Earth-Surface Processes, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/73738e2a91b7a54283ff28e95c346e05f98bc971

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. G. Feingold
2. Andrew Gettelman
3. Alexander Khain
4. Xiaohong Liu
5. Hugh Morrison
6. Bjorn Stevens
7. A. Nenes
8. Graeme L. Stephens

In Earth-Surface Processes

1. Alexander Khain
2. G. Feingold
3. Daniel Rosenfeld
4. H. Xue
5. Bjorn Stevens
6. Hongli Jiang
7. Graeme L. Stephens
8. S. C. Heever

In Global and Planetary Change

1. G. Feingold
2. Alexander Khain
3. Andrew Gettelman
4. Hugh Morrison
5. Xiaohong Liu
6. Bjorn Stevens
7. Graeme L. Stephens
8. A. Nenes

Citations in the corpus

• Aerosol effects on the lifetime of shallow cumulus (2006, background): “However, this simple chain of events has recently been challenged for warm stratocumulus clouds [Ackerman et al., 2004] and shallow cumulus [ Xue and Feingold, 2006; Jiang and Feingold, 2006; hereinafter referred to as XF and JF, respectively].”
• Multisensor satellite observations of aerosol effects on warm clouds (2008, background): “, 2000] and modeling studies [Xue and Feingold, 2006] support this hypothesis as well.”
• Aerosol effects on clouds, precipitation, and the organization of shallow cumulus convection (2008, methodology): “Similar influences of aerosol on cloud size were noted by Xue and Feingold (2006).”
• Notes on state-of-the-art investigations of aerosol effects on precipitation: a critical review (2009, background): “…McFarquhar and Heymsfield 2001, Yum and Hudson 2002, Givati and Rosenfeld 2004, Jirak and Cotton 2006, Hudson and Mishra 2007, Göke et al 2007, Xue and Feingold 2006) and numerical 1748-9326/09/015004+20$30.00 © 2009 IOP Publishing Ltd Printed in the UK1 (e.g., Khain and Pokrovsky 2004,…”
• Effect of aerosol on warm convective clouds: Aerosol‐cloud‐surface flux feedbacks in a new coupled large eddy model (2006, background): “This subject is explored further in Xue and Feingold [2006] .”
• Aerosol Indirect Effects on Tropical Convection Characteristics under Conditions of Radiative-Convective Equilibrium (2011, methodology): “The enhanced CCN concentrations in these large-scale simulations therefore do not result in greater low cloud fractions, as suggested by the second AIE, and are more in keeping with the findings of Xue and Feingold (2006) and Jiang et al. (2006).”
• Online coupled regional meteorology chemistry models in Europe: current status and prospects (2013, background): “The importance of such effects and the associated changes in cloud dynamics has been discussed by several authors (e.g. Jiang et al., 2006; Xue and Feingold, 2006).”
• Constraining the aerosol influence on cloud fraction (2016, background): “, 2013]; cloud resolving models indicate that aerosols may have a very small [Stevens and Seifert, 2008] or even slightly negative [Xue and Feingold, 2006; Seifert et al., 2015] influence on the CF of shallow cumulus clouds.”
• 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).”
• Droplet nucleation: Physically‐based parameterizations and comparative evaluation (2011, background): “Other studies of such effects have been conducted using cloud models with size-resolved bin microphysics [Fridlind et al., 2004; Khain et al., 2004; Xue and Feingold, 2006; Fan et al., 2007, 2009; Li et al., 2008], which require explicit prediction of supersaturation and are much more computationall”
• Constraining the aerosol influence on cloud liquid water path (2018, background): “(c) Evaporation–entrainment feedbacks (Wang et al., 2003; Xue and Feingold, 2006; Jiang et al., 2006; Small et al., 2009; Dagan et al., 2017) – smaller droplets have a faster evaporation timescale, enhancing the cooling and hence the negative buoyancy at the edge of cumulus clouds.”
• Review of Aerosol–Cloud Interactions: Mechanisms, Significance, and Challenges (2016, methodology): “Therefore, droplet evaporation is enhanced and the feedback between evaporation– entrainment is enhanced as well (Xue and Feingold 2006).”
• Can aerosol decrease cloud lifetime? (2009, background): “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,”