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Volume 19 Issue 5

Sep.  2002

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Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 2002 >  19(5): 767-776

Application of Linear Thermodynamics to the Atmospheric System.Part Ⅱ: Exemplification of Linear Phenomenological Relations in the Atmospheric System

  • 1.

    Coldand Aril Re gion s Environmenl and Engineering lnstitle, Chinese Academy of Sciences Lanzhou 730000;Resource Environment College of Lanzhou Unicerity, Lanzhou 730000


doi: 10.1007/s00376-002-0043-7

  • The linear phenomenological relations in the atmospheric boundary layer are proved indirectly usingobservational facts to combine linear thermodynamic theory and similarity theory in the boundary layer.Furthermore, it is proved that the turbulent transport coefficients are in proportion to the correspondinglinear phenomenological coefficients. But the experimental facts show that the linear phenomenological rela-tions are not tenable in the atmospheric mixing layer because the turbalent transport process is an intensenon-linear process in the mixing layer. Hence the convection boundary layer is a thermodynamic state in anon-linear region far from the equilibrium state. The geostrophic wind is a special cross-coupling phenom-enon between the dynamic process and the thermodynamic process in the atmospheric system. It is a practi-cal exemplification ofa cross-coupling phenomenon in the atmospheric system.
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    [2] HU Yinqiao, ZUO Hongchao, 2003: The Influence of Convergence Movement on Turbulent Transportation in the Atmospheric Boundary Layer, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 794-798.  doi: 10.1007/BF02915404
    [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
    [4] LIU Shuhua, YUE Xu, HU Fei, LIU Huizhi, 2004: Using a Modified Soil-Plant-Atmosphere Scheme (MSPAS) to Simulate the Interaction between Land Surface Processes and Atmospheric Boundary Layer in Semi-Arid Regions, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 245-259.  doi: 10.1007/BF02915711
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    • Manuscript History

    Manuscript received: 10 September 2002
    Manuscript revised: 10 September 2002
    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

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    Application of Linear Thermodynamics to the Atmospheric System.Part Ⅱ: Exemplification of Linear Phenomenological Relations in the Atmospheric System

    • 1. Coldand Aril Re gion s Environmenl and Engineering lnstitle, Chinese Academy of Sciences Lanzhou 730000;Resource Environment College of Lanzhou Unicerity, Lanzhou 730000
    • Manuscript received: 2002-09-10
    • Manuscript revised: 2002-09-10

    Abstract: The linear phenomenological relations in the atmospheric boundary layer are proved indirectly usingobservational facts to combine linear thermodynamic theory and similarity theory in the boundary layer.Furthermore, it is proved that the turbulent transport coefficients are in proportion to the correspondinglinear phenomenological coefficients. But the experimental facts show that the linear phenomenological rela-tions are not tenable in the atmospheric mixing layer because the turbalent transport process is an intensenon-linear process in the mixing layer. Hence the convection boundary layer is a thermodynamic state in anon-linear region far from the equilibrium state. The geostrophic wind is a special cross-coupling phenom-enon between the dynamic process and the thermodynamic process in the atmospheric system. It is a practi-cal exemplification ofa cross-coupling phenomenon in the atmospheric system.

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