An Improved Mellor–Yamada Level-3 Model: Its Numerical Stability and Application to a Regional Prediction of Advection Fog

By M. Nakanishi, H. Niino. 2006

1,317 citations recorded by the source corpus.

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

View Paper: https://www.semanticscholar.org/paper/d4f13ba7e5860dec1c74332c17d2adcbcfa237b3

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Citations in the corpus

Nonhydrostatic Atmospheric Models and Operational Development at JMA (2007, methodology): “As for the turbulent model, a Mellor and Yamada level 3 closure model (MY3; Nakanishi and Niino 2004, 2006) will be first implemented as the operational NWP model to reduce model 7 Similar idealized experiment for hybrid coordinate is given in Schar et al. (2002). errors in boundary layer.”
The Non-hydrostatic Icosahedral Atmospheric Model: description and development (2014, methodology): “For physical processes, we have actively introduced more sophisticated schemes, especially for cloud microphysics (Grabowski 1998; Tomita 2008b; Seiki and Nakajima 2014) and PBL schemes (Nakanishi and Niino 2006, 2009; Noda et al. 2010).”
Modulation of Wind-Work by Oceanic Current Interaction with the Atmosphere (2016, background): “5) planetary boundary layer (PBL) scheme (Nakanishi and Niino 2006).”
Modeling and Forecasting the Onset and Duration of Severe Radiation Fog under Frost Conditions (2010, background): “The study of fog with mesoscale models has been mainly concerned with advection fog over sea or in coastal regions (Ballard et al. 1991; Pagowski et al. 2004; Fu et al. 2006; Nakanishi and Niino 2006).”
The Challenge of Forecasting the Onset and Development of Radiation Fog Using Mesoscale Atmospheric Models (2015, methodology): “The sensitivity runs apply the Mellor-Yamada-Nakanishi-Niino 2.5 (MYNN) scheme (Nakanishi and Niino 2006) and the single-moment schemes WSM3 and WSM6.”
Mesoscale Data Assimilation for a Local Severe Rainfall Event with the NHM–LETKF System (2014, background): “Previous studies have pointed out that the warm and moist southwesterly wind was a key factor in increasing the precipitation near the baiu front (e.g., Davidson et al. 1998; Ninomiya 2000).”
The AFWA dust emission scheme for the GOCART aerosol model in WRF-Chem v3.8.1 (2019, neutral): “…1 Surface model Noah (Tewari et al., 2004) sf_surface_physics 2 Surface layer MM5 (Beljaars, 1994) sf_sfclay_physics 1 Boundary layer MYNN 2.5 (Nakanishi and Niino, 2006) bl_pbl_physics 5 Radiation (SW and LW) RRTMG (Iacono et al., 2008) ra_sw(lw)_physics 4 Microphysics Thompson (Thompson et…”