Turbulence, Condensation, and Liquid Water Transport in Numerically Simulated Nonprecipitating Stratocumulus Clouds.

By Shouping Wang, Qing Wang, G. Feingold. 2003

160 citations recorded by the source corpus.

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

View Paper: https://www.semanticscholar.org/paper/a3c0aa2388bf9a6615e3b91a822fd7cca0d5fdba

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. H. Xue
3. Bjorn Stevens
4. Hongli Jiang
5. Andrew Gettelman
6. Graeme L. Stephens
7. Johannes Quaas
8. E. Gryspeerdt

In Earth-Surface Processes

1. G. Feingold
2. H. Xue
3. Bjorn Stevens
4. Hongli Jiang
5. Graeme L. Stephens
6. J. Small
7. P. Chuang
8. Johannes Quaas

In Global and Planetary Change

1. G. Feingold
2. H. Xue
3. Bjorn Stevens
4. Andrew Gettelman
5. Hongli Jiang
6. Graeme L. Stephens
7. Johannes Quaas
8. E. Gryspeerdt

Citations in the corpus

• Multisensor satellite observations of aerosol effects on warm clouds (2008, methodology): “Furthermore, modeling studies [Ackerman et al., 2004], [Wang et al., 2003] frequently D R A F T March 14, 2008, 11:52am D R A F T LEBSOCK ET AL.”
• Bounding Global Aerosol Radiative Forcing of Climate Change (2020, background): “…1989), while radiation, evaporation, and sedimentation enhance cloud-top turbulence and1127 increase cloud top cooling, enhancing the entrainment of dry air, resulting in a reduc-1128 tion in L in polluted regions (S. Wang et al., 2003; A. S. Ackerman et al., 2004; Brether-1129 ton et al., 2007).”
• 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…”
• Constraining the aerosol influence on cloud liquid water path (2018, background): “, 2018), while other studies suggest a very weak LWP response to aerosol (Wang et al., 2012; Malavelle et al., 2017).”
• Aerosol effects on clouds, precipitation, and the organization of shallow cumulus convection (2008, background): “This decrease occurs entirely in the upper stratiform layer and is consistent with the shorter evaporative time scales of smaller drops as described by Xue and Feingold (2006). The relatively small difference in both cloud-averaged ql and net condensation in the stratiform layer between these two no”
• Aerosol effects on the lifetime of shallow cumulus (2006, background): “[11] Wang et al. [2003] showed that the smaller droplets associated with polluted clouds evaporate more readily and cause higher cloud-top entrainment in stratocumulus.”