SENSITIVITY OF BOUNDARY LAYER PARAMETERIZATIONS TO ATMOSPHERIC STABILITY PRECEDING HEAVY RAINFALL OCCURRED AT KANTO ON 15 AUGUST 2005

[1]  Z. Janjic.  The Step-Mountain Eta Coordinate Model: Further Developments of the Convection, Viscous Sublayer, and Turbulence Closure Schemes , 1994 .

[2]  J. Garratt.  The Atmospheric Boundary Layer , 1992 .

[3]  H. Pan,et al.  Nonlocal Boundary Layer Vertical Diffusion in a Medium-Range Forecast Model , 1996 .

[4]  J. Dudhia,et al.  Coupling an Advanced Land Surface–Hydrology Model with the Penn State–NCAR MM5 Modeling System. Part I: Model Implementation and Sensitivity , 2001 .

[5]  Da-Lin Zhang,et al.  Diurnal cycles of surface winds and temperatures as simulated by five boundary layer parameterizations , 2004 .

[6]  Da‐Lin Zhang,et al.  A High-Resolution Model of the Planetary Boundary Layer—Sensitivity Tests and Comparisons with SESAME-79 Data , 1982 .

[7]  Zavisa Janjic,et al.  The Step-Mountain Coordinate: Physical Package , 1990 .

[8]  C. Paulson.  The Mathematical Representation of Wind Speed and Temperature Profiles in the Unstable Atmospheric Surface Layer , 1970 .

[9]  Shiyuan Zhong,et al.  Sensitivity of MM5-Simulated Boundary Layer Characteristics to Turbulence Parameterizations , 2005 .

[10]  G. Grell,et al.  A description of the fifth-generation Penn State/NCAR Mesoscale Model (MM5) , 1994 .

[11]  Steven L. Mullen,et al.  The Sensitivity of the Numerical Simulation of the Southwest Monsoon Boundary Layer to the Choice of PBL Turbulence Parameterization in MM5 , 2002 .

[12]  Yuki Honda,et al.  An Assimilation and Forecasting Experiment of the Nerima Heavy Rainfa11 with a Cloud-Resolving Nonhydrostatic 4-Dimensional Variational Data Assimilation System , 2007 .

[13]  G. Mellor,et al.  Development of a turbulence closure model for geophysical fluid problems , 1982 .

[14]  Nelson L. Seaman,et al.  Evaluation of Numerical Predictions of Boundary Layer Structure during the Lake Michigan Ozone Study , 2000 .