On the kinetic energy budget of the unstable atmospheric surface layer

被引:20
|
作者
McNaughton, KG [1 ]
机构
[1] Univ Edinburgh, Sch Geosci, Edinburgh EH9 3JN, Midlothian, Scotland
基金
英国自然环境研究理事会;
关键词
turbulence; convective boundary layer; fractal; inactive motion; Monin-Obukhov similarity;
D O I
10.1007/s10546-005-3779-7
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
We present a new account of the kinetic energy budget within an unstable atmospheric surface layer (ASL) beneath a convective outer layer. It is based on the structural model of turbulence introduced by McNaughton (Boundary-Layer Meteorology, 112: 199-221, 2004). In this model the turbulence is described as a self-organizing system with a highly organized structure that resists change by instability. This system is driven from above, with both the mean motion and the large-scale convective motions of the outer layer creating shear across the surface layer. The outer convective motions thus modulate the turbulence processes in the surface layer, causing variable downwards fluxes of momentum and kinetic energy. The variable components of the momentum flux sum to zero, but the associated energy divergence is cumulative, increasing both the average kinetic energy of the turbulence in the surface layer and the rate at which that energy is dissipated. The tendency of buoyancy to preferentially enhance the vertical motions is opposed by pressure reaction forces, so pressure production, which is the work done against these reaction forces, exactly equals buoyant production of kinetic energy. The pressure potential energy that is produced is then redistributed throughout the layer through many conversions, back and forth, between pressure potential and kinetic energy with zero sums. These exchanges generally increase the kinetic energy of the turbulence, the rate at which turbulence transfers momentum and the rate at which it dissipates energy, but does not alter its overall structure. In this model the velocity scale for turbulent transport processes in the surface layer is (kz epsilon)(1/3) stop rather than the friction velocity, u(*). Here k is the von Karman constant, z is observation height, epsilon is the dissipation rate. The model agrees very well with published experimental results, and provides the foundation for the new similarity model of the unstable ASL, replacing the older Monin-Obukhov similarity theory, whose assumptions are no longer tenable.
引用
收藏
页码:83 / 107
页数:25
相关论文
共 50 条
  • [42] Estimates of the turbulent kinetic energy budget in the oceanic convective boundary layer
    Takahiro Endoh
    Takeshi Matsuno
    Yutaka Yoshikawa
    Eisuke Tsutsumi
    [J]. Journal of Oceanography, 2014, 70 : 81 - 90
  • [43] Estimates of the turbulent kinetic energy budget in the oceanic convective boundary layer
    Endoh, Takahiro
    Matsuno, Takeshi
    Yoshikawa, Yutaka
    Tsutsumi, Eisuke
    [J]. JOURNAL OF OCEANOGRAPHY, 2014, 70 (01) : 81 - 90
  • [44] The impact of Red Sea and topography on the atmospheric kinetic energy budget of a cyclonic system
    Al-Mutairi, Motirh
    Basset, Heshmat Abdel
    Abdeldym, Abdallah
    Morsy, Mostafa
    [J]. DYNAMICS OF ATMOSPHERES AND OCEANS, 2022, 98
  • [45] A NOTE ON THE KINETIC-ENERGY BUDGET ANALYSIS OF THE ATMOSPHERIC BAROCLINIC AND BAROTROPIC FLOWS
    CHEN, TC
    YEN, MC
    [J]. JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN, 1985, 63 (04) : 685 - 693
  • [46] Turbulent Kinetic Energy Dissipation in the Surface Layer
    Charuchittipan, D.
    Wilson, J. D.
    [J]. BOUNDARY-LAYER METEOROLOGY, 2009, 132 (02) : 193 - 204
  • [47] Turbulent Kinetic Energy Dissipation in the Surface Layer
    D. Charuchittipan
    J. D. Wilson
    [J]. Boundary-Layer Meteorology, 2009, 132 : 193 - 204
  • [48] TURBULENCE REYNOLDS-NUMBER AND THE TURBULENT KINETIC-ENERGY BALANCE IN THE ATMOSPHERIC SURFACE-LAYER
    BRADLEY, EF
    ANTONIA, RA
    CHAMBERS, AJ
    [J]. BOUNDARY-LAYER METEOROLOGY, 1981, 21 (02) : 183 - 197
  • [49] SURFACE-LAYER AND ENERGY BUDGET PARAMETERIZATIONS FOR MESOSCALE MODELS
    NICKERSON, EC
    SMILEY, VE
    [J]. JOURNAL OF APPLIED METEOROLOGY, 1975, 14 (03): : 297 - 300
  • [50] Sound propagation in an unstable atmospheric layer
    Naugolnykh, K. A.
    Rybak, S. A.
    [J]. ACOUSTICAL PHYSICS, 2007, 53 (03) : 417 - 420