A New Vertical Diffusion Package with an Explicit Treatment of Entrainment Processes

By Song‐You Hong, Y. Noh, Jimy Dudhia. 2006

6,500 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/5a27ff42aeebc7218c89c0bc4e47a63a4d3c2d6e

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In Global and Planetary Change

Citations in the corpus

Evaluation of Planetary Boundary Layer Parameterizations in Tropical Cyclones by Comparison of In Situ Observations and High-Resolution Simulations of Hurricane Isabel (2003). Part I: Initialization, Maximum Winds, and the Outer-Core Boundary Layer (2009, methodology): “The Yonsei University scheme (Noh et al. 2003; Hong et al. 2006) is an updated and improved version of the scheme previously known as the ‘‘MRF’’ scheme, based on its use in the Medium-Range Forecast model at the National Centers for Environmental Prediction (NCEP) (Hong and Pan 1996).”
Moisture and dynamical interactions maintaining decoupled Arctic mixed-phase stratocumulus in the presence of a humidity inversion (2011, methodology): “Planetary boundary Yonsei University scheme (non-local-K scheme with explicit entrainment layer layer mixing package and parabolic K profile in unstable mixed layers) in 5 and 25 km grids Hong et al. (2006).”
Evaluation of cloud‐resolving and limited area model intercomparison simulations using TWP‐ICE observations: 1. Deep convective updraft properties (2014, background): “…Figuresa LAM Simulation Configurations Simulation Symbol Domain (D4) Δx (m) Δz (m) Microphysics WRF-W Triangle 450 km × 330 km 1000 ~100–300 One moment [Hong et al., 2006] WRF-T Square 450 km × 330 km 1000 ~100–300 Two moment (r) [Thompson et al., 2008] WRF-M Diamond 450 km × 330 km 1000 ~100–300…”
Intercomparison of Planetary Boundary-Layer Parametrizations in the WRF Model for a Single Day from CASES-99 (2011, methodology): “7a of Hong et al. 2006).”
A Review of Planetary Boundary Layer Parameterization Schemes and Their Sensitivity in Simulating Southeastern U.S. Cold Season Severe Weather Environments (2015, neutral): “The parameterization of the PBL by these models directly inﬂuences the models’ portrayal of buoyancy and vertical wind shear, as well as precipitation evolution (e.g., Hong et al. 2006).”
A Revised Scheme for the WRF Surface Layer Formulation (2012, methodology): “The PBL is parameterized with the Yonsei University scheme (Hong et al. 2006) with the first model level that defines the surface layer at 28 m (h 5 0.993).”
The dependence of aerosol effects on clouds and precipitation on cloud‐system organization, shear and stability (2008, methodology): “[2006], Khain et al. [2005], and Lynn et al. [2005] showed increasing precipitation for deep convection, associated with increases of aerosol number concentration and, thereby, CCN.”
Cloud‐resolving model intercomparison of an MC3E squall line case: Part I—Convective updrafts (2017, methodology): “We use the Rapid Radiative Transfer Model for application to GCMs shortwave and longwave radiation schemes [Iacono et al., 2008], the Noah Land Surface Model [Chen and Dudhia, 2001], and the Mellor–Yamada–Janjic (MYJ) planetary boundary layer scheme [Hong et al., 2006].”
Development of an Improved Turbulence Closure Model for the Atmospheric Boundary Layer (2009, methodology): “First-order turbulence closure models, such as the K-profile model (e.g., Troen and Mahrt 1986; Hong et al. 2006), the KE (so-called one-anda-half order closure) model (e.g., Therry and Lacarrère 1983; Bougeault and Lacarrère 1989), and the standard k e model (e.g., Hanjalic and Launder 1972),…”
Simulating North American mesoscale convective systems with a convection-permitting climate model (2017, methodology): “The main physics packages used in our WRF simulation are the Thompson aerosol-aware microphysics (Thompson and Eidhammer 2014), the Yonsei University (YSU) planetary boundary layer scheme (Hong et al. 2006), the Rapid Radiative Transfer Model (RRTMG) (Iacono et al.”
Nested Mesoscale Large-Eddy Simulations with WRF: Performance in Real Test Cases (2012, methodology): “The PBL dynamics in mesoscale runs are simulated using the Yonsei University PBL scheme (Noh et al. 2003; Hong et al. 2006)—referred to as YSU PBL.”