Size Statistics of Cumulus Cloud Populations in Large-Eddy Simulations
By R. Neggers, DeBilt, theNetherlands, Harm J. J. Jonker, A. P. Siebesma. 2003
150 citations recorded by the source corpus.
Subfields: Earth-Surface Processes, Environmental Engineering, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/e253042f46629249ebe104098426045c7325736c
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In Earth-Surface Processes
In Environmental Engineering
- Anton Beljaars
- Martin Köhler
- R. Neggers
- G. Feingold
- Bjorn Stevens
- C. V. Heerwaarden
- Harm J. J. Jonker
- T. Heus
In Global and Planetary Change
Citations in the corpus
- Large-Eddy Simulations of Trade Wind Cumuli: Investigation of Aerosol Indirect Effects (2006, methodology): “the cloud (Neggers et al. 2003), where the area of the”
- The Distribution of Cloud Horizontal Sizes (2011, background): “While this is not a new point (see, e.g., Neggers et al. 2003), Fig.”
- Large‐eddy simulations over Germany using ICON: a comprehensive evaluation (2017, result): “These slopes appear steeper than those reported in previous studies (e.g. between −1.7 and 2.0 from Neggers et al. (2003) and Dawe and Austin (2012), based on domain sizes of 6.4 km) but remain consistent with those obtained from larger LES simulations (e.g. around −2.7 from Heus and Seifert (2013)…”
- Large‐eddy simulation of the transient and near‐equilibrium behavior of precipitating shallow convection (2015, unknown): “A similar scale break has been identified in simulations [e.g., Neggers et al., 2003] and also in observations through the analysis of echo objects as measured during RICO [Trivej and Stevens, 2010], although quantitative the details of the scale break depends somewhat on the details of SEIFERT ET…”
- Formulation of the Dutch Atmospheric Large-Eddy Simulation (DALES) and overview of its applications (2010, methodology): “In a recent effort, DALES is being used in the KNMI Parameterization Testbed (Neggers et al., 2010), which allows for a day-by-day comparison between observational data, LES, and large-scale model results.”
- A Dual Mass Flux Framework for Boundary Layer Convection. Part I: Transport (2009, methodology): “Small Cumulus Microphysics Study Knight and Miller (1998) and French et al. (1999) Neggers et al. (2003a) top and convective cloud base coincide; the reason for this simplification is that the transition layer depth dtr cannot be expected to be well resolved at present-day GCMs for which this…”