Article Contents

EXPERIMENTS OF A REDUCED GRID IN LASG/IAPWORLD OCEANGENERAL CIRCULATION MODELS (OGCMs)

Funding:

  • Due to the decrease in grid size associated with the convergence of meridians toward the poles in spherical coordinates, the time steps in many global climate models with finite-difference method are restricted to be unpleasantly small. To overcome the problem, a reduced grid is introduced to LASG/IAP world ocean general circulation models. The reduced grid is implemented successfully in the coarser resolutions version model L30T63 at first. Then, it is carried out in the improved version model LICOM with finer resolutions. In the experiment with model L30T63, under time step unchanged though, execution time per single model run is shortened significantly owing to the decrease of grid number and filtering execution in high latitudes. Results from additional experiments with L30T63 show that the time step of integration can be quadrupled at most in reduced grid with refinement ratio 3. In the experiment with model LICOM and with the model’s original time step unchanged, the model covered area is extended to the whole globe from its original case with the grid point of North Pole considered as an isolated island and the results of experiment are shown to be acceptable.
  • [1] WANG Bin, WAN Hui, JI Zhong-zhen, et al. Design of anew dynamical core for global atmospheric models based onsome efficient numerical methods [J]. Science in China, 2004,47(Supp.): 4-21.
    [2] KUO H L, NORDO J. Integration of four-level prognosticequations over the hemisphere [J]. Tellus, 1959, 11: 412-424.
    [3] GATES W L, RIEGEL C A. A study of numerical errors in the integration of barotropic flow on a spherical grid [J].Journal of geophysical research, 1962, 67: 773-784.
    [4] KURIHARA Y. Numerical integration of the primitiveequations on a spherical grid [J]. Monthly Weather Review,1965, 93: 399-415.
    [5] RASCH P J. Conservative shape-preserving twodimensionaltransport on a spherical reduced grid [J]. MonthlyWeather Review, 1994, 122: 1337-1350.
    [6] WICKETT M E, DUFFY P B, RODRIGUE G.. A reducedgrid for a parallel global ocean general circulation model [J].Ocean Modelling, 2000, 2: 85-107.
    [7] JIN Xiang-ze, ZHANG Xue-hong, ZHOU Tian-jun.Fundamental framework and experiments of the thirdgeneration of IAP/LASG world ocean general circulation model[J]. Advances in Atmospheric Sciences, 1999, 16:
    [8] LIU Hai-long. Improvements on an OGCM and simulationof ocean surface flow [D]. Beijing: Institute of AtmosphericPhysics, Chinese Academy of Sciences, 2002.
    [9] ZHANG Xue-hong, LIANG Xin-zhong. A numerical worldocean general circulation model [J]. Advances in AtmosphericSciences, 1989, 6: 43-61.
    [10] CHEN Ke-ming. Improvement on IAP coupled oceanatmospheregeneral circulation model and simulation ofgradually increasing CO2 induced climate change [D]. Beijing:Institute of Atmospheric Physics, Chinese Academy of Sciences,1994.197-215.
    [11] ZHANG Xue-hong, CHEN Ke-ming, JIN Xiang-ze, et al.Simulation of thermohaline circulation with a twenty-layeroceanic general circulation model [J]. Theoretical and AppliedClimatology, 1996, 55: 65-87.
    [12] YU Yong-qiang. Design of ocean-sea ice-atmospherecoupling scheme and numerical simulation of interdecadalclimate variability [D]. Beijing: Institute of AtmosphericPhysics, Chinese Academy of Sciences, 1997.
    [13] YU Yong-qiang, ZHANG Xue-hong. Acoupling scheme ofair-sea anomaly flux [M]// Study and Design of OperationalDynamic Model for Short-Range Climate Prediction System.Beijing: China Meteorological Press, 2000. 201-207.
    [14] YU Yong-qiang, LIU Xi-ying. ENSO and Indian Oceandipole mode in three coupled GCMs [J]. Acta OceanologicaSinica, 2004, 23:581-595.
    [15] LIU Xi-ying. Simulation of sea-sea ice-air interaction inhigh northern latitudes [D]. Beijing: Institute of AtmosphericPhysics, Chinese Academy of Sciences, 2001.
    [16] ZHANG Xue-hong, YU Yong-qiang, LIU Hai-long. TheDevelopment and Application of the Oceanic GeneralCirculation Model in LASG/IAP: I. the Global OceanicGeneral Circulation Model [J]. Chinese Journal ofAtmospheric Sciences, 2003, 27: 607-617.
    [17] LIU Hai-long, YU Yong-qiang, LI Wei, et al. ReferenceManual of LASG/IAP Climate System Ocean Model(LICOM1.0) [M]// Special technical report of State KeyLaboratory of Numerical Modelling for Atmospheric Sciencesand Geophysical Fluid Dynamics, Beijing: Science Press, 2004.1-7.
    [18] STEELE M, MORLEY R, ERMOLD W. PHC: A globalocean hydrography with a high quality Arctic Ocean [J].Journal of Climate, 2001, 14: 2079-2087.

Get Citation+

LIU Xi-ying, LIU Hai-long, ZHANG Xue-hong, et al. EXPERIMENTS OF A REDUCED GRID IN LASG/IAPWORLD OCEANGENERAL CIRCULATION MODELS (OGCMs) [J]. Journal of Tropical Meteorology, 2006, 12(1): 9-15.
LIU Xi-ying, LIU Hai-long, ZHANG Xue-hong, et al. EXPERIMENTS OF A REDUCED GRID IN LASG/IAPWORLD OCEANGENERAL CIRCULATION MODELS (OGCMs) [J]. Journal of Tropical Meteorology, 2006, 12(1): 9-15.
Export:  

Share Article

Manuscript History

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

EXPERIMENTS OF A REDUCED GRID IN LASG/IAPWORLD OCEANGENERAL CIRCULATION MODELS (OGCMs)

Abstract: Due to the decrease in grid size associated with the convergence of meridians toward the poles in spherical coordinates, the time steps in many global climate models with finite-difference method are restricted to be unpleasantly small. To overcome the problem, a reduced grid is introduced to LASG/IAP world ocean general circulation models. The reduced grid is implemented successfully in the coarser resolutions version model L30T63 at first. Then, it is carried out in the improved version model LICOM with finer resolutions. In the experiment with model L30T63, under time step unchanged though, execution time per single model run is shortened significantly owing to the decrease of grid number and filtering execution in high latitudes. Results from additional experiments with L30T63 show that the time step of integration can be quadrupled at most in reduced grid with refinement ratio 3. In the experiment with model LICOM and with the model’s original time step unchanged, the model covered area is extended to the whole globe from its original case with the grid point of North Pole considered as an isolated island and the results of experiment are shown to be acceptable.

LIU Xi-ying, LIU Hai-long, ZHANG Xue-hong, et al. EXPERIMENTS OF A REDUCED GRID IN LASG/IAPWORLD OCEANGENERAL CIRCULATION MODELS (OGCMs) [J]. Journal of Tropical Meteorology, 2006, 12(1): 9-15.
Citation: LIU Xi-ying, LIU Hai-long, ZHANG Xue-hong, et al. EXPERIMENTS OF A REDUCED GRID IN LASG/IAPWORLD OCEANGENERAL CIRCULATION MODELS (OGCMs) [J]. Journal of Tropical Meteorology, 2006, 12(1): 9-15.
Reference (18)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return