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
  • [22] Measurement of turbulence near shear-free density interfaces
    Kit, ELG
    Strang, EJ
    Fernando, HJS
    JOURNAL OF FLUID MECHANICS, 1997, 334 : 293 - 314
  • [23] A NUMERICAL STUDY ON THE FORMATION OF A THERMOCLINE IN SHEAR-FREE TURBULENCE
    NOH, Y
    FERNANDO, HJS
    PHYSICS OF FLUIDS A-FLUID DYNAMICS, 1991, 3 (03): : 422 - 426
  • [24] Comments on "Langmuir Turbulence and Surface Heating in the Ocean Surface Boundary Layer''
    Noh, Yign
    Choi, Yeonju
    JOURNAL OF PHYSICAL OCEANOGRAPHY, 2018, 48 (02) : 455 - 458
  • [25] Effects of turbulence and heterogeneous emissions on photochemically active species in the convective boundary layer
    Krol, MC
    Molemaker, MJ
    de Arellano, JVG
    JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2000, 105 (D5) : 6871 - 6884
  • [26] Entrainment in a shear-free turbulent mixing layer
    Briggs, DA
    Ferziger, JH
    Koseff, JR
    Monismith, SG
    JOURNAL OF FLUID MECHANICS, 1996, 310 : 215 - 241
  • [27] MODEL OF WIND SHEAR AND TURBULENCE IN THE SURFACE BOUNDARY LAYER.
    Luers, James K.
    NASA Contractor Reports, 1973,
  • [28] On vortex formation in multicell convective clouds in a shear-free environment
    Shapiro, A.
    Kogan, Y. L.
    ATMOSPHERIC RESEARCH, 1994, 33 (1-4) : 125 - 136
  • [29] Surface fluxes under shear-free convection
    Akylas, E
    Tombrou, M
    Lalas, D
    Zilitinkevich, SS
    QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2001, 127 (574) : 1183 - 1197
  • [30] Reply to "Comments on 'Langmuir Turbulence and Surface Heating in the Ocean Surface Boundary Layer"'
    Pearson, Brodie C.
    Grant, Alan L. M.
    Polton, Jeff A.
    Belcher, Stephen E.
    JOURNAL OF PHYSICAL OCEANOGRAPHY, 2018, 48 (02) : 459 - 462