A Combined Local and Nonlocal Closure Model for the Atmospheric Boundary Layer. Part I: Model Description and Testing

By J. Pleim. 2007

973 citations recorded by the source corpus.

Subfields: Atmospheric Science, Environmental Engineering

View Paper: https://www.semanticscholar.org/paper/d8f9d4fd257cf8313d6f9c8fe6b7c9440074e87b

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In Environmental Engineering

Citations in the corpus

Verification of Convection-Allowing WRF Model Forecasts of the Planetary Boundary Layer Using Sounding Observations (2013, methodology): “This result suggests that the use of local mixing under more stable regimes in the ACM2 scheme (Pleim 2007) consistently produces more accurate nocturnal PBL depths than the YSU scheme.”
Representation of the Subgrid-Scale Turbulent Transport in Convective Boundary Layers at Gray-Zone Resolutions (2015, background): “The conventional nonlocal PBL parameterizations express the nonlocal transport through a mass-ﬂux term (e.g., Pleim 2007; Siebesma et al. 2007; Pergaud et al. 2009) or a gradient-adjustment gamma term (e.g., Troen and Mahrt 1986; Holtslag and Boville 1993; Hong et al. 2006).”
Intercomparison of Planetary Boundary-Layer Parametrizations in the WRF Model for a Single Day from CASES-99 (2011, methodology): “In the ACM2 scheme, the method is similar to that of the YSU scheme; h is diagnosed as the height above the level of neutral buoyancy where the bulk Richardson number for the entrainment layer exceeds the critical value (Pleim 2007b).”
Seasonal variation of local atmospheric circulations and boundary layer structure in the Beijing‐Tianjin‐Hebei region and implications for air quality (2015, methodology): “…four commonly used BL schemes (i.e., the Yonsei University (YSU) [Hong et al., 2006; Hu et al., 2013], Mellor-Yamada-Janjic (MYJ) [Janjić, 1994], Bougeault-Lacarrere (Boulac) [Bougeault and Lacarr ere, 1989], and Asymmetric Convective Model, version 2 (ACM2) [Pleim, 2007] schemes) were tested.”
Impact of aerosol–meteorology interactions on fine particle pollution during China’s severe haze episode in January 2013 (2014, methodology): “…(Kain 2004), the Asymmetric Convective Model version 2 for the PBL (Pleim 2007a, 2007b), the RRTMG radiation mechanism and the Pleim–Xiu land-surface model (Pleim and Xiu 1995 and Xiu and Pleim 2001) with indirect soil moisture and temperature nudging (Pleim and Xiu 2003, Pleim and Gilliam 2009).”
A Description of the Advanced Research WRF Version 3 (2008, methodology): “The ACM2 (Pleim, 2007) is a combination of the ACM, which is a simple transilient model that was originally a modification of the Blackadar convective model, and an eddy diffusion model.”
A Description of the Advanced Research WRF Model Version 4 (2019, methodology): “88 8.6.4 Mellor-Yamada-Nakanishi-Niino (MYNN) Levels 2.5 and 3 . . . . . . . . 88 8.6.5 Asymmetrical Convective Model version 2 (ACM2) PBL . . . . . . . . . 89 8.6.6 Bougeault-Lacarrere PBL . . . . . . . . . . . . . . . . . . . . . . . . . .”