Cloud resolving modeling of the ARM summer 1997 IOP: Model formulation, results, uncertainties, and sensitivities

By M. Khairoutdinov, David A. Randall. 2003

976 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/b0752472113877159a460931e6a48df5519105db

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Citations in the corpus

The Role of Convective Moistening in the Madden–Julian Oscillation (2009, background): “Details of the formulation of the CRM can be found in Khairoutdinov and Randall (2003), and more information on its implementation within the CAM can be found in Khairoutdinov and Randall (2001), Khairoutdinov et al. (2005, and 2008).”
Self‐aggregation of convection in long channel geometry (2014, positive): “15 K and a weighted average of the two between those temperatures, consistent with the thermodynamics of SAM (Khairoutdinov and Randall, 2003).”
Intercomparison of cloud model simulations of Arctic mixed‐phase boundary layer clouds observed during SHEBA/FIRE‐ACE (2011, background): “Model Investigator(s) and model reference Cloud microphysics Prognostic cloud variables Dimensionality, Horizontal gridspacing, domain size # of vertical levels in the BL1 DHARMA Ann Fridlind bin microphysics 32 liquid and 32 ice bins 3D 43 Andy Ackerman Ackerman et al. (1995) 50 m Ackerman et al. (”
Influence of the subcloud layer on the development of a deep convective ensemble (2012, methodology): “As in Khairoutdinov and Randall (2003), an additional graupel class was used for precipitation.”
Physical mechanisms controlling self‐aggregation of convection in idealized numerical modeling simulations (2013, methodology): “[15] The model used is the System for Atmospheric Modeling, version 6.8.2, henceforth referred to as SAM [Khairoutdinov and Randall, 2003].”
Effects of aerosol optical properties on deep convective clouds and radiative forcing (2008, background): “Several previous studies have also concluded that, although some aspects of 2-D simulations differ from 3-D simulations, many important statistical characteristics, such as mean temperature and water profile, cloud fraction, and precipitation rates, etc., tend to be similar [ Khairoutdinov and Randa”
A New Moist Turbulence Parameterization in the Community Atmosphere Model (2009, methodology): “The SAM is described in Khairoutdinov and Randall (2003) and was kindly provided to us by Dr.”
Simulations of the Atmospheric General Circulation Using a Cloud-Resolving Model as a Superparameterization of Physical Processes (2005, methodology): “The SP component of the SP-CAM is a modified version of a three-dimensional (3D) CRM described in detail by Khairoutdinov and Randall (2003).”
A Mass-Flux Scheme View of a High-Resolution Simulation of a Transition from Shallow to Deep Cumulus Convection (2006, methodology): “We use the System for Atmospheric Modeling (SAM), which is an updated version of the Colorado State University Large Eddy Simulation / Cloud Resolving Model (Khairoutdinov and Randall, 2003).”
Observations of Clouds, Aerosols, Precipitation, and Surface Radiation over the Southern Ocean: An Overview of CAPRICORN, MARCUS, MICRE, and SOCRATES (2020, methodology): “Table ES13 lists some modeling groups that participated in the projects, as well as the approximate grid resolution; additional details about the LES simulations are also included in the online supplement.”
Large‐Eddy Simulation of Maritime Deep Tropical Convection (2009, methodology): “The model used in this study is the System for Atmospheric Modeling (SAM; version 6.7) documented by Khairoutdinov and Randall (2003).”
Simulations of midlatitude frontal clouds by single-column and cloud--resolving models during the Atmospheric Radiation Measurement March 2000 cloud intensive operational period (2005, positive): “Earlier studies [e.g., Grabowski et al., 1998; Khairoutdinov and Randall, 2003] showed that 2-D and 3-D CRMs could generally produce similar statistical”
High-Resolution Simulation of Shallow-to-Deep Convection Transition over Land (2006, methodology): “The cloud-resolving model used in this study is the System for Atmospheric Modeling (SAM; Khairoutdinov and Randall 2003).”
An Energy-Balance Analysis of Deep Convective Self-Aggregation above Uniform SST (2005, methodology): “The readers are referred to Khairoutdinov and Randall (2003) for further details about the model.”