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Volume 13 Issue 2

Apr.  1996

Article Contents
Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 1996 >  13(2): 169-182

A 2-D Non-local Closure Model for Atmospheric Boundary Layer Simulations

  • 1.

    Guest Researcher in LAPC, Beijing 100029,Guest Researcher in LAPC, Beijing 100029


doi: 10.1007/BF02656860

  • In this paper a new approach for PBL simulation, the non-local closure scheme based on the transient turbu-lence theory has been used. It was set up as an alternative to local closure schemes which physical concept is reasona-ble and distinct. A 2-D non-local closure model was developed in order to study the PBL structure and simulate some interesting atmospheric processes over non-uniform underlying surface, especially under the convective and unique weather conditions, such as sea-land circulation and the TIBL structure. The modelled results show good agreement with field measurement.
  • [1] Chen Panqin, 1985: NUMERICAL SIMULATION FOR THE EFFECTS OF PBL AND THE SURFACE ON POLLUTANT CONCENTRATIONS, ADVANCES IN ATMOSPHERIC SCIENCES, 2, 251-259.  doi: 10.1007/BF03179757
    [2] Xun ZHU, 2003: Parameterization of the Non-Local Thermodynamic Equilibrium Source Function with Chemical Production by an Equivalent Two-Level Model, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 487-495.  doi: 10.1007/BF02915493
    [3] GAO Zhiqiu, BIAN Lingen, CHEN Zhigang, Michael SPARROW, ZHANG Jiahua, 2006: Turbulent Variance Characteristics of Temperature and Humidity over a Non-uniform Land Surface for an Agricultural Ecosystem in China, ADVANCES IN ATMOSPHERIC SCIENCES, 23, 365-374.  doi: 10.1007/s00376-006-0365-y
    [4] Yu Zhihao, Chen Liangdong, 1985: THE INFLUENCE OF HORIZONTALLY NON-UNIFORM HEATING UPON THE DEVELOPMENT OF STRONG CONVECTIVE MESOSCALE DISTURBANCES, ADVANCES IN ATMOSPHERIC SCIENCES, 2, 347-358.  doi: 10.1007/BF02677251
    [5] Zhao Ming, 1988: THE NUMERICAL EXPERIMENTS ON APPLICATING GEOSTROPHIC MOMENTUM APPROXIMATION TO THE BAROCLINIC AND NON-NEUTRAL PBL, ADVANCES IN ATMOSPHERIC SCIENCES, 5, 287-300.  doi: 10.1007/BF02656753
    [6] Chao LIU, Li FU, Dan YANG, David R. MILLER, Junming WANG, 2020: Non-Gaussian Lagrangian Stochastic Model for Wind Field Simulation in the Surface Layer, ADVANCES IN ATMOSPHERIC SCIENCES, 37, 90-104.  doi: 10.1007/s00376-019-9052-7
    [7] Shi Yong, Jiang Weimei, 1998: The Numerical Simulation on the PBL Structure and Its Evolution over Small-Scale Concave Terrain, ADVANCES IN ATMOSPHERIC SCIENCES, 15, 99-106.  doi: 10.1007/s00376-998-0021-9
    [8] Yuqiang SONG, Hongnian LIU, Xueyuan WANG, Ning ZHANG, Jianning SUN, 2016: Numerical Simulation of the Impact of Urban Non-uniformity on Precipitation, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 783-793.  doi: 10.1007/s00376-016-5042-1
    [9] LI Wanli, LU Shihua, FU Shenming, MENG Xianhong, H. C. NNAMCHI, 2011: Numerical Simulation of Fluxes Generated by Inhomogeneities of the Underlying Surface over the Jinta Oasisin Northwestern China, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 887-906.  doi: 10.1007/s00376-010-0041-0
    [10] Al-Jiboori M. H., Xu Yumao, Qian Yongfu, 2000: Local Similarity Relationships of Non-Dimensional Wind and Temperature Gradient in the Tower-Layer Atmosphere over Beijing City, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 636-648.  doi: 10.1007/s00376-000-0025-6
    [11] Wenshou TIAN, GUO Zhenhai, YU Rucong, 2004: Treatment of LBCs in 2D Simulation of Convection over Hills, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 573-586.  doi: 10.1007/BF02915725
    [12] Zhao Ming, 1988: A NUMERICAL EXPERIMENT OF THE PBL WITH GEO-STROPHIC MOMENTUM APPROXIMATION, ADVANCES IN ATMOSPHERIC SCIENCES, 5, 47-56.  doi: 10.1007/BF02657345
    [13] ZHAO Qiaohua, SUN Jihua, ZHU Guangwei, 2012: Simulation and Exploration of the Mechanisms Underlying the Spatiotemporal Distribution of Surface Mixed Layer Depth in a Large Shallow Lake, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 1360-1373.  doi: 10.1007/s00376-012-1262-1
    [14] Qian Yongfu, Wang Qianqian, 1984: A NUMERICAL SIMULATION OF D1URNA1 VARIATIONS OF METEOROLOGICAL FIELDS IN SUMMER, ADVANCES IN ATMOSPHERIC SCIENCES, 1, 40-61.  doi: 10.1007/BF03187615
    [15] Guo Weidong, Sun Shufen, Qian Yongfu, 2002: Case Analyses and Numerical Simulation of Soil Thermal Impacts on Land Surface Energy Budget Based on an Off-Line Land Surface Model, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 500-512.  doi: 10.1007/s00376-002-0082-0
    [16] Chen Ming, Hong Zhongxiang, Arnaldo Longhetto, Richiardone Renzo, 1996: Sensitivity Study of Nonlocal Turbulence Closure Scheme in Local Circulation, ADVANCES IN ATMOSPHERIC SCIENCES, 13, 147-158.  doi: 10.1007/BF02656858
    [17] Chen Jiabin, Wang Jun, 1996: Studies on Non-interpolating Semi-Lagrangian Scheme and Numerical Solution to KdV Equation, ADVANCES IN ATMOSPHERIC SCIENCES, 13, 265-268.  doi: 10.1007/BF02656869
    [18] LI Xiaohan, PENG Xindong, LI Xingliang, 2015: An Improved Dynamic Core for a Non-hydrostatic Model System on the Yin-Yang Grid, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 648-658.  doi: 10.1007/s00376-014-4120-5
    [19] Yifan ZHAO, Xindong PENG, Xiaohan LI, Siyuan CHEN, 2024: Improved Diurnal Cycle of Precipitation on Land in a Global Non-Hydrostatic Model Using a Revised NSAS Deep Convective Scheme, ADVANCES IN ATMOSPHERIC SCIENCES.  doi: 10.1007/s00376-023-3121-7
    [20] Xun Zhu, 1989: A Parameterization of Cooling Rate Calculation under the Non-LTE Condition: Multi-Level Model, ADVANCES IN ATMOSPHERIC SCIENCES, 6, 403-413.  doi: 10.1007/BF02659075
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    • Manuscript History

    Manuscript received: 10 April 1996
    Manuscript revised: 10 April 1996
    通讯作者: 陈斌, bchen63@163.com
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    A 2-D Non-local Closure Model for Atmospheric Boundary Layer Simulations

    • 1. Guest Researcher in LAPC, Beijing 100029,Guest Researcher in LAPC, Beijing 100029
    • Manuscript received: 1996-04-10
    • Manuscript revised: 1996-04-10

    Abstract: In this paper a new approach for PBL simulation, the non-local closure scheme based on the transient turbu-lence theory has been used. It was set up as an alternative to local closure schemes which physical concept is reasona-ble and distinct. A 2-D non-local closure model was developed in order to study the PBL structure and simulate some interesting atmospheric processes over non-uniform underlying surface, especially under the convective and unique weather conditions, such as sea-land circulation and the TIBL structure. The modelled results show good agreement with field measurement.

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