Parameterization of entrainment in a sheared convective boundary layer using a first-order jump model

被引:36
作者
Kim, Si-Wan
Park, Soon-Ung
Pino, David
Vila-Guerau de Arellano, Jordi
机构
[1] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[2] Seoul Natl Univ, Sch Earth & Environm Sci, Seoul, South Korea
[3] Tech Univ Catalonia, Dept Appl Phys, Barcelona, Spain
[4] Inst Space Studies Catalonia, Barcelona, Spain
[5] Univ Wageningen & Res Ctr, Meterol & Air Qual Sect, Wageningen, Netherlands
[6] Natl Ocean & Atmospher Adm, Div Chem Sci, Earth Syst Res Lab, Boulder, CO 80305 USA
关键词
entrainment heat flux; first-order jump model; inversion layer depth; large-eddy simulation; sheared convective boundary layer;
D O I
10.1007/s10546-006-9067-3
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Basic entrainment equations applicable to the sheared convective boundary layer (CBL) are derived by assuming an inversion layer with a finite depth, i.e., the first-order jump model. Large-eddy simulation data are used to determine the constants involved in the parameterizations of the entrainment equations. Based on the integrated turbulent kinetic energy budget from surface to the top of the CBL, the resulting entrainment heat flux normalized by surface heat flux is a function of the inversion layer depth, the velocity jumps across the inversion layer, the friction velocity, and the convection velocity. The developed first-order jump model is tested against large-eddy simulation data of two independent cases with different inversion strengths. In both cases, the model reproduces quite reasonably the evolution of the CBL height, virtual potential temperature, and velocity components in the mixed layer and in the inversion layer.
引用
收藏
页码:455 / 475
页数:21
相关论文
共 47 条
[1]   An evaluation of neutral and convective planetary boundary-layer parameterizations relative to large eddy simulations [J].
Ayotte, KW ;
Sullivan, PP ;
Andren, A ;
Doney, SC ;
Holtslag, AAM ;
Large, WG ;
Mcwilliams, JC ;
Moeng, CH ;
Otte, MJ ;
Tribbia, JJ ;
Wyngaard, JC .
BOUNDARY-LAYER METEOROLOGY, 1996, 79 (1-2) :131-175
[2]   NON-PRECIPITATING CUMULUS CONVECTION AND ITS PARAMETERIZATION [J].
BETTS, AK .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1973, 99 (419) :178-196
[3]   First International Satellite Land Surface Climatology Field Experiment 1987 sonde budget revisited [J].
Betts, AK ;
Barr, AG .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D18) :23285-23288
[4]  
BOERS R, 1984, J CLIM APPL METEOROL, V23, P247, DOI 10.1175/1520-0450(1984)023<0247:LOOMLD>2.0.CO
[5]  
2
[6]  
CONZEMIUS R, 2004, P 16 C BOUND LAYER T
[7]  
Cuijpers JWM, 1998, J ATMOS SCI, V55, P151, DOI 10.1175/1520-0469(1998)055<0151:IOSANE>2.0.CO
[8]  
2
[9]  
DEARDORFF JW, 1972, MON WEATHER REV, V100, P93, DOI 10.1175/1520-0493(1972)100<0093:POTPBL>2.3.CO
[10]  
2