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Volume 13 Issue 2

Apr.  1996

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Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 1996 >  13(2): 229-243

Comparison of Surface Wind Stress Anomalies over the Tropical Pacific Simulated by an AGCM and by a Simple Atmospheric Model

  • 1.

    Department of Atmospheric Sciences, Nanjing University, Nanjing 210093,Lamont-Doherty Earth Observatory of Columbia University, Palisades, N. Y. 10964, U.S.A,Lamont-Doherty Earth Observatory of Columbia University, Palisades, N. Y. 10964, U.S.A,Center for Ocean-Land-Atmosphere Studies Calverton, MD 20705-2425, U.S.A


doi: 10.1007/BF02656865

  • In this paper, surface wind stress anomalies over the tropical Pacific simulated by an AGCM and by a simple at-mospheric model are compared with observed. The AGCM is the higher resolution global spectral model-COLA R40 model and the simple atmospheric model is the atmospheric component of the Cane-Zebiak coupled ocean-at-mosphere model The results show that the wind stress anomalies simulated by both the COLA R40 and the simple model have captured the main features of observation but the x component in the CZ model is closer to that in observation than that in the COLA model, and the correlation coefficients between simulated SSTA from the CZ model and observed for Nino indices are higher than those from the COLA model.
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    [2] 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
    [3] Ni Yunqi, Zhang Qin, 1996: Low Frequency Characteristics of Tropical Pacific Wind Stress Anomalies in Observations and Simulations from a Simple and a Comprehensive Models, ADVANCES IN ATMOSPHERIC SCIENCES, 13, 445-460.  doi: 10.1007/BF03342036
    [4] Zeng Qingcun, Dai Yongjiu, Xue Feng, 1998: Simulation of the Asian Monsoon by IAP AGCM Coupled with an Advanced Land Surface Model (IAP94), ADVANCES IN ATMOSPHERIC SCIENCES, 15, 1-16.  doi: 10.1007/s00376-998-0013-9
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    [10] Dai Yongjiu, Xue Feng, Zeng Qingcun, 1998: A Land Surface Model (IAP94) for Climate Studies Part II: Implementation and Preliminary Results of Coupled Model with IAP GCM, ADVANCES IN ATMOSPHERIC SCIENCES, 15, 47-62.  doi: 10.1007/s00376-998-0017-5
    [11] Wang Huijun, 1997: The Effect of Heating Anomaly on the Asian Circulation-A GCM Experiment, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 81-86.  doi: 10.1007/s00376-997-0046-5
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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
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

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    Comparison of Surface Wind Stress Anomalies over the Tropical Pacific Simulated by an AGCM and by a Simple Atmospheric Model

    • 1. Department of Atmospheric Sciences, Nanjing University, Nanjing 210093,Lamont-Doherty Earth Observatory of Columbia University, Palisades, N. Y. 10964, U.S.A,Lamont-Doherty Earth Observatory of Columbia University, Palisades, N. Y. 10964, U.S.A,Center for Ocean-Land-Atmosphere Studies Calverton, MD 20705-2425, U.S.A
    • Manuscript received: 1996-04-10
    • Manuscript revised: 1996-04-10

    Abstract: In this paper, surface wind stress anomalies over the tropical Pacific simulated by an AGCM and by a simple at-mospheric model are compared with observed. The AGCM is the higher resolution global spectral model-COLA R40 model and the simple atmospheric model is the atmospheric component of the Cane-Zebiak coupled ocean-at-mosphere model The results show that the wind stress anomalies simulated by both the COLA R40 and the simple model have captured the main features of observation but the x component in the CZ model is closer to that in observation than that in the COLA model, and the correlation coefficients between simulated SSTA from the CZ model and observed for Nino indices are higher than those from the COLA model.

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