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Volume 8 Issue 2

Mar.  1991

Article Contents

Influence of Advection on Marine PBL Development


doi: 10.1007/BF02658094

  • Based on the DRS model (one coupled dynamical-radiational model of stratocumulus), though extended to take advection into account, several calculations have been made to estimate its contributions to the thermodynamical structure of the PBL (planetary boundary layer). Advection various calvulations show does affect the development of the PBL, Particularly in cloud forming and evolving. One of the intriguing findings which accords well with observations demonstrates that cold currents create strong convective weather, while warm currents bring about stable weather: produce prolonged low clouds or fogs.
  • [1] Wang Ling, Xu Yinzi, 1997: The Influence of Weakly-Nonlinear Vertical Advection on the Wind Field of PBL with Large-Scale Orography, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 59-68.  doi: 10.1007/s00376-997-0044-7
    [2] 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
    [3] 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
    [4] ZHAO Chunsheng, Yutaka ISHIZAKA, 2004: Modeling Marine Stratocumulus with a Detailed Microphysical Scheme, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 61-74.  doi: 10.1007/BF03342546
    [5] ZHAO Chunsheng, Yutaka ISHIZAKA, WU Guoxiong, WANG Huijun, Da-Lin ZHANG, 2004: Retraction:Modeling Marine Stratocumulus with a Detailed Microphysical Scheme, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 382-382.  doi: 10.1007/BF03342548
    [6] Zhao Bolin, Zhen Jinming, Hu Chengda, Du Jinlin, Zhu Yuanjing, Zhang Chengxiang, 1992: Study on Clouds and Marine Atmospheric Boundary Layer, ADVANCES IN ATMOSPHERIC SCIENCES, 9, 383-396.  doi: 10.1007/BF02677072
    [7] ZHANG Kai, WAN Hui, WANG Bin, ZHANG Meigen, 2008: Consistency Problem with Tracer Advection in the Atmospheric Model GAMIL, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 306-318.  doi: 10.1007/s00376-008-0306-z
    [8] 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
    [9] WANG Dongxiao, QIN Zenghao, SHI Ping, 2004: Progress in Marine Meteorology Studies in China during 1999-2002, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 485-496.  doi: 10.1007/BF02915575
    [10] James E. OVERLAND, Muyin WANG, Thomas J. BALLINGER, 2018: Recent Increased Warming of the Alaskan Marine Arctic Due to Midlatitude Linkages, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 75-84.  doi: 10.1007/s00376-017-7026-1
    [11] WANG Dongxiao, ZHANG Yan, ZENG Lili, LUO Lin, 2009: Marine Meteorology Research Progress of China from 2003 to 2006, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 17-30.  doi: 10.1007/s00376-009-0017-0
    [12] Xiang SONG, Xiaodong ZENG, Jiawen ZHU, Pu SHAO, 2016: Development of an Establishment Scheme for a DGVM, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 829-840.  doi: 10.1007/s00376-016-5284-y
    [13] Xiaofan Li, Han-Ru Cho, 1997: Development and Propagation of Equatorial Waves, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 323-338.  doi: 10.1007/s00376-997-0053-6
    [14] WU Xiandu, RAN Lingkun, CHU Yanli, 2011: Diagnosis of a Moist Thermodynamic Advection Parameter in Heavy-Rainfall Events, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 957-972.  doi: 10.1007/s00376-009-9057-8
    [15] Luo Zhexian, 1994: Study of Effects of Beta Term and Nonlinear Advection on the Structure of Tropical Cyclones, ADVANCES IN ATMOSPHERIC SCIENCES, 11, 391-398.  doi: 10.1007/BF02658158
    [16] Yu Rucong, 1994: A Two-Step Shape-Preserving Advection Scheme, ADVANCES IN ATMOSPHERIC SCIENCES, 11, 479-490.  doi: 10.1007/BF02658169
    [17] 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
    [18] 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
    [19] ZHAO Bin, ZHONG Qing, 2010: The Development of a Nonhydrostatic Global Spectral Model, ADVANCES IN ATMOSPHERIC SCIENCES, 27, 676-684.  doi: 10.1007/s00376-009-9080-9
    [20] Pan Xiaoling, Chao Jiping, 2001: The Effects of Climate on Development of Ecosystem in Oasis, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 42-52.  doi: 10.1007/s00376-001-0003-7

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Manuscript History

Manuscript received: 10 March 1991
Manuscript revised: 10 March 1991
通讯作者: 陈斌, bchen63@163.com
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Influence of Advection on Marine PBL Development

  • 1. Institute of Atmospheric Physics, Academia Sinica, Beijing 100029, China

Abstract: Based on the DRS model (one coupled dynamical-radiational model of stratocumulus), though extended to take advection into account, several calculations have been made to estimate its contributions to the thermodynamical structure of the PBL (planetary boundary layer). Advection various calvulations show does affect the development of the PBL, Particularly in cloud forming and evolving. One of the intriguing findings which accords well with observations demonstrates that cold currents create strong convective weather, while warm currents bring about stable weather: produce prolonged low clouds or fogs.

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