Small-Scale and Mesoscale Variability in Cloudy Boundary Layers: Joint Probability Density Functions

By V. Larson, J. Golaz, William Cotton. 2002

175 citations recorded by the source corpus.

Subfields: Atmospheric Science, Environmental Engineering, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/8460b4bc37c4b3a40d00fc50a0c806a4a85252d5

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. Andrew Gettelman
2. J. Golaz
3. Hugh Morrison
4. V. Larson
5. Xiaohong Liu
6. P. Bogenschutz
7. Richard B. Neale
8. Peter M. Caldwell

In Environmental Engineering

1. V. Larson
2. J. Golaz
3. William Cotton
4. Hugh Morrison
5. P. Bogenschutz
6. Andrew Gettelman
7. Cheryl Craig
8. D. P. Schanen

In Global and Planetary Change

1. Andrew Gettelman
2. J. Golaz
3. Hugh Morrison
4. V. Larson
5. Xiaohong Liu
6. P. Bogenschutz
7. Peter M. Caldwell
8. Richard B. Neale

Citations in the corpus

• A PDF-Based Model for Boundary Layer Clouds. Part I: Method and Model Description (2002, methodology): “The procedure in these cases is detailed in Larson et al. (2002).”
• Using Probability Density Functions to Derive Consistent Closure Relationships among Higher-Order Moments (2005, methodology): “There are plausible sets of moments that are specifically unrealizable with respect to the Analytic Double Gaussian 1 family of Larson et al. (2002), because this PDF family is too restrictive.”
• Understanding Cloud and Convective Characteristics in Version 1 of the E3SM Atmosphere Model (2018, unknown): “CLUBB assumes a PDF shape that is double Gaussian, which allows for both stratocumulus and cumulus clouds to be represented with a single PDF (Bogenschutz et al., 2010; Larson et al., 2002).”
• A PDF-Based Model for Boundary Layer Clouds. Part II: Model Results (2002, methodology): “The family of PDFs employed is the three-dimensional analytic double Gaussian 1 family proposed by Larson et al. (2002).”
• An Overview of the Atmospheric Component of the Energy Exascale Earth System Model (2019, methodology): “The PDF is assumed to have a normal mixture (i.e., double Gaussian) shape using the Analytic Double Gaussian 1 shape of Larson et al. (2002).”
• Higher-Order Turbulence Closure and Its Impact on Climate Simulations in the Community Atmosphere Model (2013, methodology): “For a complete formulation of closure assumptions used for some of these terms please refer to Golaz et al. (2007) and Larson et al. (2002, 2012).”