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Volume 24 Issue 1

Jan.  2007

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Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 2007 >  24(1): 89-100

Principle of Cross Coupling Between Vertical Heat Turbulent Transport and Vertical Velocity and Determination of Cross Coupling Coefficient

  • 1.

    College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000; Cold and Arid Regions Environment and Engineering Institute, Chinese Academy of Sciences, Gansu Province Key Laboratory of Arid Climatic Change and Reducing Disaster, Lanzhou 730000; Department of Environment and Resource, Gansu Agriculture University, Lanzhou 730060,College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000; Cold and Arid Regions Environment and Engineering Institute, Chinese Academy of Sciences, Gansu Province Key Laboratory of Arid Climatic Change and Reducing Disaster, Lanzhou 730000,College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000


doi: 10.1007/s00376-007-0089-7

  • It has been proved that there exists a cross coupling between vertical heat turbulent transport and vertical velocity by using linear thermodynamics. This result asserts that the vertical component of heat turbulent transport flux is composed of both the transport of the vertical potential temperature gradient and the coupling transport of the vertical velocity. In this paper, the coupling effect of vertical velocity on vertical heat turbulent transportation is validated by using observed data from the atmospheric boundary layer to determine cross coupling coefficients, and a series of significant properties of turbulent transportation are opened out. These properties indicate that the cross coupling coefficient is a logarithm function of the dimensionless vertical velocity and dimensionless height, and is not only related to the friction velocity u*, but also to the coupling roughness height zW0 and the coupling temperature TW0 of the vertical velocity. In addition, the function relations suggest that only when the vertical velocity magnitude conforms to the limitation |W/u*|≠1, and is above the level zW0, then the vertical velocity leads to the cross coupling effect on the vertical heat turbulent transport flux. The cross coupling theory and experimental results provide a challenge to the traditional turbulent K closure theory and the Monin-Obukhov similarity theory.
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    [2] Hu Yinqiao, 2002: Application of Linear Thermodynamics to the Atmospheric System.Part Ⅱ: Exemplification of Linear Phenomenological Relations in the Atmospheric System, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 767-776.  doi: 10.1007/s00376-002-0043-7
    [3] ZHOU Li, XU Xiangde, DING Guoan, ZHOU Mingyu, CHENG Xinghong, 2005: Diurnal Variations of Air Pollution and Atmospheric Boundary Layer Structure in Beijing During Winter 2000/2001, ADVANCES IN ATMOSPHERIC SCIENCES, 22, 126-132.  doi: 10.1007/BF02930876
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    • Manuscript History

    Manuscript received: 10 January 2007
    Manuscript revised: 10 January 2007
    通讯作者: 陈斌, bchen63@163.com
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    Principle of Cross Coupling Between Vertical Heat Turbulent Transport and Vertical Velocity and Determination of Cross Coupling Coefficient

    • 1. College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000; Cold and Arid Regions Environment and Engineering Institute, Chinese Academy of Sciences, Gansu Province Key Laboratory of Arid Climatic Change and Reducing Disaster, Lanzhou 730000; Department of Environment and Resource, Gansu Agriculture University, Lanzhou 730060,College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000; Cold and Arid Regions Environment and Engineering Institute, Chinese Academy of Sciences, Gansu Province Key Laboratory of Arid Climatic Change and Reducing Disaster, Lanzhou 730000,College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000
    • Manuscript received: 2007-01-10
    • Manuscript revised: 2007-01-10

    Abstract: It has been proved that there exists a cross coupling between vertical heat turbulent transport and vertical velocity by using linear thermodynamics. This result asserts that the vertical component of heat turbulent transport flux is composed of both the transport of the vertical potential temperature gradient and the coupling transport of the vertical velocity. In this paper, the coupling effect of vertical velocity on vertical heat turbulent transportation is validated by using observed data from the atmospheric boundary layer to determine cross coupling coefficients, and a series of significant properties of turbulent transportation are opened out. These properties indicate that the cross coupling coefficient is a logarithm function of the dimensionless vertical velocity and dimensionless height, and is not only related to the friction velocity u*, but also to the coupling roughness height zW0 and the coupling temperature TW0 of the vertical velocity. In addition, the function relations suggest that only when the vertical velocity magnitude conforms to the limitation |W/u*|≠1, and is above the level zW0, then the vertical velocity leads to the cross coupling effect on the vertical heat turbulent transport flux. The cross coupling theory and experimental results provide a challenge to the traditional turbulent K closure theory and the Monin-Obukhov similarity theory.

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