Advanced Search

Volume 3 Issue 3

Jul.  1986

Article Contents

A GLOBAL MODEL WITH OVERLAPPING MERCATOR AND STEREOGRAPHIC GRIDS


doi: 10.1007/BF02678651

  • A global nine-layer primitive equation model is developed to investigate the dynamic and thermodynamic influences of plateaus and high mountains on the atmospheric circulation. Besides topography, the effects of solar radiation, longwave radiation, large-scale condensation, cumulus convection and surface fluxes of heat momentum are also included in the model, In order that the finite-difference approximations represent fairly accurately the circulation in both higher and lower latitudes, we use Mercator projection in lower latitudes and Stereographic projection in higher latitudes.The simulated sea level pressure, wind field, precipitation distribution and vertical circulation in summer and winter are given, respectively, and they are compared with the observations.
  • [1] Liu Yudi, Ji Zhongzhen, Wang Bin, 2002: Study on Computational Properties of Several Vertical Grids with a Nonhydrostatic Model in Comparison to Analytical Solutions, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 528-543.  doi: 10.1007/s00376-002-0084-y
    [2] LI Xingliang, SHEN Xueshun, PENG Xindong, XIAO Feng, ZHUANG Zhaorong, CHEN Chungang, 2013: An Accurate Multimoment Constrained Finite Volume Transport Model on Yin-Yang Grids, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 1320-1330.  doi: 10.1007/s00376-013-2217-x
    [3] 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
    [4] LIU Yudi, WANG Bin, JI Zhongzhen, 2003: Research on Atmospheric Motion in Horizontal Discrete Grids, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 139-148.  doi: 10.1007/BF03342058
    [5] Shi Guangyu, 1984: EFFECT OF ATMOSPHERIC OVERLAPPING BANDS AND THEIR TREATMENT ON THE CALCULATION OF THERMAL RADIATION, ADVANCES IN ATMOSPHERIC SCIENCES, 1, 246-262.  doi: 10.1007/BF02678137
    [6] ZENG Xiaodong, LI Fang, SONG Xiang, 2014: Development of the IAP Dynamic Global Vegetation Model, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 505-514.  doi: 10.1007/s00376-013-3155-3
    [7] Zhang Daomin, Li Jinlong, Ji Liren, Huang Boyin, Wu Wanli, Chen Jiabin, Song Zhengshan, 1995: A Global Spectral Model and Test of Its Performance, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 67-78.  doi: 10.1007/BF02661288
    [8] WangHuijun, Xue Feng, Bi Xunqiang, 1997: The Interannual Variability and Predictability in a Global Climate Model, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 554-562.  doi: 10.1007/s00376-997-0073-2
    [9] Zhou Jiabin, 1984: THE APPLICATION OF CHEBYSHEV POLYNOMIALS IN IRREGULAR GRIDS IN THE FORECAST OF PRECIPITATION DISTRIBUTION, ADVANCES IN ATMOSPHERIC SCIENCES, 1, 206-223.  doi: 10.1007/BF02678133
    [10] Huan MEI, Faming WANG, Zhong ZENG, Zhouhua QIU, Linmao YIN, Liang LI, 2016: A Global Spectral Element Model for Poisson Equations and Advective Flow over a Sphere, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 377-390.  doi: 10.1007/s00376-015-5001-2
    [11] XU Yongfu, LI Yangchun, and CHU Min, 2013: A Global Ocean Biogeochemistry General Circulation Model and its Simulations, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 922-939.  doi: 10.1007/s00376-012-2162-0
    [12] Zhang Renjian, Wang Mingxing, Zeng Qingcun, 2000: Global Two-Dimensional Chemistry Model and Simulation of Atmospheric Chemical Composition, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 72-82.  doi: 10.1007/s00376-000-0044-3
    [13] Li Yinpeng, Ji Jinjun, 2001: Model Estimates of Global Carbon Flux between Vegetation and the Atmosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 807-818.
    [14] Yueliang CHEN, Changxiang YAN, Jiang ZHU, 2018: Assimilation of Sea Surface Temperature in a Global Hybrid Coordinate Ocean Model, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 1291-1304.  doi: 10.1007/s00376-018-7284-6
    [15] Jiawen ZHU, Xiaodong ZENG, Minghua ZHANG, Yongjiu DAI, Duoying JI, Fang LI, Qian ZHANG, He ZHANG, Xiang SONG, 2018: Evaluation of the New Dynamic Global Vegetation Model in CAS-ESM, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 659-670.  doi: 10.1007/s00376-017-7154-7
    [16] XU Yongfu, LI Yangchun, 2009: Estimates of Anthropogenic CO2 Uptake in a Global Ocean Model, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 265-274.  doi: 10.1007/s00376-009-0265-z
    [17] Chen Jiabin, Ji Liren, Wu Wanli, 1987: DESIGN AND TEST OF AN IMPROVED SCHEME FOR GLOBAL SPECTRAL MODEL WITH REDUCED TRUNCATION ERROR, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 156-168.  doi: 10.1007/BF02677062
    [18] Sheng Hua, William Bourke, Terry Hart, 1992: An Impact of Hydrostatic Extraction Scheme on BMRC’s Global Spectral Model, ADVANCES IN ATMOSPHERIC SCIENCES, 9, 269-278.  doi: 10.1007/BF02656937
    [19] Zhang Ronghua, Zeng Qingcun, Zhou Guangqing, Liang Xinzhong, 1995: A Coupled General Circulation Model for the Tropical Pacific Ocean and Global Atmosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 127-142.  doi: 10.1007/BF02656827
    [20] ZENG Xiaodong, 2010: Evaluating the Dependence of Vegetation on Climate in an Improved Dynamic Global Vegetation Model, ADVANCES IN ATMOSPHERIC SCIENCES, 27, 977-991.  doi: 10.1007/s00376-009-9186-0

Get Citation+

Export:  

Share Article

Manuscript History

Manuscript received: 10 July 1986
Manuscript revised: 10 July 1986
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

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

A GLOBAL MODEL WITH OVERLAPPING MERCATOR AND STEREOGRAPHIC GRIDS

  • 1. Department of Earth and Space Sciences, University of Science and Technology of China, Hefei,Department of Geophysical Sciences, The University of Chicago, Chicago, IL 60637 U.S.A.

Abstract: A global nine-layer primitive equation model is developed to investigate the dynamic and thermodynamic influences of plateaus and high mountains on the atmospheric circulation. Besides topography, the effects of solar radiation, longwave radiation, large-scale condensation, cumulus convection and surface fluxes of heat momentum are also included in the model, In order that the finite-difference approximations represent fairly accurately the circulation in both higher and lower latitudes, we use Mercator projection in lower latitudes and Stereographic projection in higher latitudes.The simulated sea level pressure, wind field, precipitation distribution and vertical circulation in summer and winter are given, respectively, and they are compared with the observations.

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return