Simulations of Trade Wind Cumuli under a Strong Inversion

By Bjorn Stevens, Andrew, Ackerman, Bruce, Albrecht, Brown, A. Chlond, Joan Cuxart, Peter, Duynkerke and 7 more. 2001

282 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/4f27ddae4dd9c254def928fa226eb18b162ff8c3

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Citations in the corpus

Marine Boundary Layer Cloud Feedbacks in a Constant Relative Humidity Atmosphere (2012, background): “Our decision to focus on this case, as opposed to other trade wind cases in the literature (e.g., Stevens et al. 2001; Siebesma et al. 2003; Stevens 2007; Bellon and Stevens 2012) is motivated by several factors.”
Aerosol effects on clouds, precipitation, and the organization of shallow cumulus convection (2008, methodology): “As in the ATEX intercomparison study (Stevens et al. 2001), a simple Beer’s law radiation scheme is used to represent the net export of radiant energy, F x, y, z, t F0 exp z ql dz , 1 where is the basic-state air density, ql is the liquid water mixing ratio, F0 74 W m 2, and 130 m2 kg 1.”
Evaluation of Large-Eddy Simulations via Observations of Nocturnal Marine Stratocumulus (2005, background): “Past studies have shown that for averaging times significantly longer than the eddy turnover time, differences among independent, identically configured simulations are negligible (e.g., Stevens et al. 2001).”
Controls on precipitation and cloudiness in simulations of trade‐wind cumulus as observed during RICO (2011, methodology): “Likewise our understanding of lateral entrainment through the sides of shallow cumulus (Siebesma and Cuijpers, 1995) has been consolidated through a series of case studies developed by the GCSS (Stevens et al., 2001; Siebesma et al., 2003).”
A Large Eddy Simulation Intercomparison Study of Shallow Cumulus Convection (2003, background): “…Berekely National Laboratory / University of Washington (LBNL/ UW) NCAR Lewellen et al. (1996) Stevens et al. (1996) Khairoutdinov and Kogan (1999) Stevens et al. (2000) Moeng (1984) C2/M2 C4/M4 C4/M4 M2/M2 S-C2/S-C2 L/F L/F A/A F/F A/A TKE-SD SL-AN TKE-AN SL-AN TKE-AN * CN (MN) stands for…”
Size Statistics of Cumulus Cloud Populations in Large-Eddy Simulations (2003, background): “…intercomparison studies by the Global Energy and Water Cycle Experiment (GEWEX) Cloud Systems Studies working group 1 (GCSS wg1) have shown that LES is robust in reproducing the bulk vertical turbulent transport of the cloud ensemble (Stevens et al. 2001; Brown et al. 2002; Siebesma et al. 2003).”
Overview of the Meso-NH model version 5.4 and its applications (2018, background): “Initiated under the Global Energy and Water Cycle Experiment (GEWEX) project with the GEWEX Cloud System Study (GCSS) working group (Bechtold et al., 2000; Redelsperger et al., 2000; Stevens et al., 2001; Xie et al., 2002), many of these intercomparison studies involving Meso-NH have focused on deep”
A Combined Eddy-Diffusivity Mass-Flux Approach for the Convective Boundary Layer (2007, background): “These percentages coincide well with the area fraction of buoyant updrafts in the cloudy cores in the case of a cloud-topped boundary layer (Siebesma and Cuijpers 1995; Stevens et al. 2001; Brown et al. 2002; Siebesma et al. 2003).”
Large‐eddy simulation of the diurnal cycle of shallow cumulus convection over land (2002, methodology): “This is consistent with past experience (e.g. Stevens et al. 2001).”