Turbulence Characteristics of the Shear-Free Convective Boundary Layer Driven by Heterogeneous Surface Heating

被引:15
|
作者
Liu, Gang [1 ]
Sun, Jianning [1 ]
Yin, Lei [1 ]
机构
[1] Nanjing Univ, Sch Atmospher Sci, Nanjing 210093, Peoples R China
关键词
Convective boundary layer; Dominant scale; Heterogeneity scale; Large-eddy simulation; Organized turbulent eddies; LARGE-EDDY SIMULATION; THERMALLY FORCED CIRCULATIONS; LAND-SURFACE; SCALE; WIND; FLUX; INHOMOGENEITIES; OSCILLATIONS; MODEL;
D O I
10.1007/s10546-011-9591-7
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Large-eddy simulations (LESs) are employed to investigate the turbulence characteristics in the shear-free convective boundary layer (CBL) driven by heterogeneous surface heating. The patterns of surface heating are arranged as a chessboard with two different surface heat fluxes in the neighbouring patches, and the heterogeneity scale I > in four different cases is taken as 1.2, 2.5, 5.0 and 10.0 km, respectively. The results are compared with those for the homogeneous case. The impact of the heterogeneity scale on the domain-averaged CBL characteristics, such as the profiles of the potential temperature and the heat flux, is not significant. However, different turbulence characteristics are induced by different heterogeneous surface heating. The greatest turbulent kinetic energy (TKE) is produced in the case with the largest heterogeneity scale, whilst the TKE in the other heterogeneous cases is close to that for the homogeneous case. This result indicates that the TKE is not enhanced unless the scale of the heterogeneous surface heating is large enough. The potential temperature variance is enhanced more significantly by a larger surface heterogeneity scale. But this effect diminishes with increasing CBL height, which implies that the turbulent eddy structures are changed during the CBL development. Analyses show that there are two types of organized turbulent eddies: one relates to the thermal circulations induced by the heterogeneous surface heating, whilst the other identifies with the inherent turbulent eddies (large eddies) induced by the free convection. At the early stage of the CBL development, the dominant scale of the organized turbulent eddies is controlled by the scale of the surface heterogeneity. With time increasing, the original pattern breaks up, and the vertical velocity eventually displays horizontal structures similar to those for the homogeneous heating case. It is found that after this transition, the values of lambda/z (i) (lambda is the dominant horizontal scale of the turbulent eddies, z (i) is the boundary-layer height) a parts per thousand 1.6, which is just the aspect ratio of large eddies in the CBL.
引用
收藏
页码:57 / 71
页数:15
相关论文
共 50 条
  • [41] Experiments on the spreading of shear-free turbulence under the influence of confinement and rotation
    Kinzel, Matthias
    Holzner, Markus
    Luethi, Beat
    Tropea, Cameron
    Kinzelbach, Wolfgang
    Oberlack, Martin
    EXPERIMENTS IN FLUIDS, 2009, 47 (4-5) : 801 - 809
  • [42] Experiments on the spreading of shear-free turbulence under the influence of confinement and rotation
    Matthias Kinzel
    Markus Holzner
    Beat Lüthi
    Cameron Tropea
    Wolfgang Kinzelbach
    Martin Oberlack
    Experiments in Fluids, 2009, 47 : 801 - 809
  • [43] SHEAR-FREE TURBULENT BOUNDARY-LAYERS .1. PHYSICAL INSIGHTS INTO NEAR-WALL TURBULENCE
    PEROT, B
    MOIN, P
    JOURNAL OF FLUID MECHANICS, 1995, 295 : 199 - 227
  • [44] The contribution of shear to the evolution of a convective boundary layer
    Pino, D
    De Arellano, JVG
    Duynkerke, PG
    JOURNAL OF THE ATMOSPHERIC SCIENCES, 2003, 60 (16) : 1913 - 1926
  • [45] The shear contribution to the evolution of a convective boundary layer
    Pino, D
    Duynkerke, PG
    de Arellano, JVG
    15TH SYMPOSIUM ON BOUNDARY LAYERS AND TURBULENCE, 2002, : 35 - 38
  • [46] Role of Convective Structures and Background Turbulence in the Dry Convective Boundary Layer
    Antti Hellsten
    Sergej Zilitinkevich
    Boundary-Layer Meteorology, 2013, 149 : 323 - 353
  • [47] Role of Convective Structures and Background Turbulence in the Dry Convective Boundary Layer
    Hellsten, Antti
    Zilitinkevich, Sergej
    BOUNDARY-LAYER METEOROLOGY, 2013, 149 (03) : 323 - 353
  • [48] FREE STREAM TURBULENCE AND SHEAR EFFECTS ON BOUNDARY-LAYER AND WAKE STRUCTURES
    LUXTON, RE
    ANTONIA, RA
    AHMAD, QA
    PHYSICS OF FLUIDS, 1977, 20 (10) : S288 - S288
  • [49] High resolution DNS of a shear-free mixing layer and LES
    Debliquy, O.
    Knaepen, B.
    Desmidts, D.
    Carati, D.
    Direct and Large-Eddy Simulation V, Proceedings, 2004, 9 : 31 - 38
  • [50] Intercomparison of Synthetic Inflow Turbulence Generation Methods in Thermally Driven Convective Boundary Layer Simulations
    Sato, Takuto
    Kusaka, Hiroyuki
    SOLA, 2023, 19 : 165 - 172