‘Application of a New Spectral Theory of Stably Stratified Turbulence to the Atmospheric Boundary Layer over Sea Ice’

By S. Sukoriansky, B. Galperin, V. Perov. 2005

324 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/27049aa0fc305d986695ab98052f187bd7f5ee91

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In Atmospheric Science

In Global and Planetary Change

Citations in the corpus

THE MARTIAN ATMOSPHERIC BOUNDARY LAYER (2011, methodology): “The QNSE‐based expressions for KM and KH have been successfully tested in both K − and K − ‘ applications [Sukoriansky et al., 2005a, 2006; Sukoriansky and Galperin, 2008].”
Intercomparison of Planetary Boundary-Layer Parametrizations in the WRF Model for a Single Day from CASES-99 (2011, methodology): “These three parametrization methods are explained in more detail in Janjić (1990) (MYJ), Sukoriansky et al. (2005) (QNSE), and Bougeault and Lacarrére (1989) (BouLac).”
Verification of Convection-Allowing WRF Model Forecasts of the Planetary Boundary Layer Using Sounding Observations (2013, methodology): “The QNSE scheme is similar to MYJ, except the diffusivities under stable conditions are calculated from spectral theory to account for internal wave generation in the presence of turbulence (Sukoriansky et al. 2005).”
Stable Atmospheric Boundary Layers and Diurnal Cycles: Challenges for Weather and Climate Models (2013, methodology): “The cases also inspired new model developments (e.g., Sukoriansky et al. 2005; Mauritsen and Svensson 2007; Buzzi et al. 2011) and are increasingly used for applications like particle dispersion (e.g., Weil 2010).”
A New Moist Turbulence Parameterization in the Community Atmosphere Model (2009, background): “For example, modification of the stability functions under highly stable stratification (e.g., following Sukoriansky et al. 2005) could improve stable boundary layer performance.”
A Description of the Advanced Research WRF Model Version 4 (2019, methodology): “This should be used with the Quasi-Normal Scale Elimination (QNSE) PBL scheme (Sukoriansky et al., 2005) named for a theoretical technique employed to derive sub-grid mixing properties of stratified turbulence.”