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Volume 9 Issue 4

Oct.  1992

Article Contents

Analysis-Prediction Experiments over Indian Region Using Primitive Equation Barotropic Model


doi: 10.1007/BF02677080

  • The impact of initial guess and grid resolutions on the analysis and prediction has been investigated over the In-dian region. For this purpose, an univariate objective analysis scheme and a primitive equation barotropic model have been used. The impact of initial guess and the resolutions on analysis and prediction is discussed.
  • [1] A. Bandyopadhyay, 1992: Split-Explicit Integration of Primitive Equation Barotropic Model for the Prediction of Movement of Monsoon Depression, ADVANCES IN ATMOSPHERIC SCIENCES, 9, 83-92.  doi: 10.1007/BF02656933
    [2] Zhu Baozhen, Chen Jiabin, Zhang Daomin, Li Zechun, Ge Aifen, 1984: AN OPERATIONAL 5-LAYER PRIMITIVE EQUATION MODEL FOR NORTHERN HEMISPHERE PREDICTION, ADVANCES IN ATMOSPHERIC SCIENCES, 1, 214-233.  doi: 10.1007/BF02678134
    [3] Liao Dongxian, 1990: A Regional Spectral Nested Multilevel Primitive Equation Model, ADVANCES IN ATMOSPHERIC SCIENCES, 7, 27-35.  doi: 10.1007/BF02919165
    [4] S. K. Sinha, D. R. Talwalkar, S. Rajamani, 1987: ON SOME ASPECTS OF OBJECTIVE ANALYSIS OF HUMI-DITY OVER INDIAN REGION BY THE OPTIMUM INTERPOLATION METHOD, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 332-342.  doi: 10.1007/BF02663603
    [5] S. K. Sinha, D, R. Talwalkar, S. G. Narkhedkar, P. L. Kulkarni, S. Nair, S. Rajamani, 1990: Use of Surface Observations to Estimate Upper Air Humidity for the Objective Analysis of Relative Humidity over Indian Region, ADVANCES IN ATMOSPHERIC SCIENCES, 7, 491-501.  doi: 10.1007/BF03342567
    [6] A. Bandyopadhyay, S.S. Singh, 1994: Evaluation of Forecast Performance of an Economical Explicit Time Integration Scheme in a Limited Area Model over Indian Region, ADVANCES IN ATMOSPHERIC SCIENCES, 11, 101-110.  doi: 10.1007/BF02656999
    [7] Ning ZHANG, Yunsong DU, Shiguang MIAO, Xiaoyi FANG, 2016: Evaluation of a Micro-scale Wind Model's Performance over Realistic Building Clusters Using Wind Tunnel Experiments, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 969-978.  doi: 10.1007/s00376-016-5273-1
    [8] Chuan GAO, Xinrong WU, Rong-Hua ZHANG, 2016: Testing a Four-Dimensional Variational Data Assimilation Method Using an Improved Intermediate Coupled Model for ENSO Analysis and Prediction, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 875-888.  doi: 10.1007/s00376-016-5249-1
    [9] ZHU Congwen, Chung-Kyu PARK, Woo-Sung LEE, Won-Tae YUN, 2008: Statistical Downscaling for Multi-Model Ensemble Prediction of Summer Monsoon Rainfall in the Asia-Pacific Region Using Geopotential Height Field, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 867-884.  doi: 10.1007/s00376-008-0867-x
    [10] Yuli ZHANG, Chuanxi LIU, Yi LIU, Rui YANG, 2019: Intraseasonal Oscillation of Tropospheric Ozone over the Indian Summer Monsoon Region, ADVANCES IN ATMOSPHERIC SCIENCES, 36, 417-430.  doi: 10.1007/s00376-018-8113-7
    [11] Zeinab SALAH, Ahmed SHALABY, Allison L. STEINER, Ashraf S. ZAKEY, Ritesh GAUTAM, Mohamed M. ABDEL WAHAB, 2018: Study of Aerosol Direct and Indirect Effects and Auto-conversion Processes over the West African Monsoon Region Using a Regional Climate Model, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 182-194.  doi: 10.1007/s00376-017-7077-3
    [12] S. K. Sinha, S. G. Narkhedkar, D. R. Talwalkar, S. Rajamani, 1992: Some Experiments with Multivariate Objective Analysis Scheme of Heights and Winds Using Optimum Interpolation, ADVANCES IN ATMOSPHERIC SCIENCES, 9, 431-440.  doi: 10.1007/BF02677075
    [13] N. R. Parija, S. K. Dash, 1995: Some Aspects of the Characteristics of Monsoon Disturbances Using a Combined Barotropic-Baroclinic Model, ADVANCES IN ATMOSPHERIC SCIENCES, 12, 487-506.  doi: 10.1007/BF02657007
    [14] Liu Shida, Liu Shikuo, 1985: NONLINEAR WAVES IN BAROTROPIC MODEL, ADVANCES IN ATMOSPHERIC SCIENCES, 2, 147-157.  doi: 10.1007/BF03179747
    [15] Chuan GAO, Rong-Hua ZHANG, Xinrong WU, Jichang SUN, 2018: Idealized Experiments for Optimizing Model Parameters Using a 4D-Variational Method in an Intermediate Coupled Model of ENSO, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 410-422.  doi: 10.1007/s00376-017-7109-z
    [16] Peihua QIN, Zhenghui XIE, Rui HAN, Buchun LIU, 2024: Evaluation and Projection of Population Exposure to Temperature Extremes over the Beijing−Tianjin−Hebei Region Using a High-Resolution Regional Climate Model RegCM4 Ensemble, ADVANCES IN ATMOSPHERIC SCIENCES.  doi: 10.1007/s00376-023-3123-5
    [17] ZHANG Ming, ZHAO Yanling, HUANG Hong, LIANG Danqing, 2007: The Generalized Energy Equation and Instability in the Two-layer Barotropic Vortex, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 147-151.  doi: 10.1007/s00376-007-0147-1
    [18] Wu Guoxiong, Chen Biao, 1989: Non-Acceleration Theorem in a Primitive Equation System: I. Acceleration of Zonal Mean Flow, ADVANCES IN ATMOSPHERIC SCIENCES, 6, 1-20.  doi: 10.1007/BF02656914
    [19] Baofeng JIAO, Lingkun RAN, Na LI, Ren CAI, Tao QU, Yushu ZHOU, 2023: Comparative Analysis of the Generalized Omega Equation and Generalized Vertical Motion Equation, ADVANCES IN ATMOSPHERIC SCIENCES, 40, 856-873.  doi: 10.1007/s00376-022-1435-5
    [20] Liu Ruizhi, 1985: NUMERICAL EXPERIMENT OF SIX-LEVEL IMPLICIT PRIMITIVE MODEL, ADVANCES IN ATMOSPHERIC SCIENCES, 2, 178-188.  doi: 10.1007/BF03179750

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Manuscript History

Manuscript received: 10 October 1992
Manuscript revised: 10 October 1992
通讯作者: 陈斌, bchen63@163.com
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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Analysis-Prediction Experiments over Indian Region Using Primitive Equation Barotropic Model

  • 1. Indain Institute of Tropical Meteorology, Pune-411008, India,Indain Institute of Tropical Meteorology, Pune-411008, India,Indain Institute of Tropical Meteorology, Pune-411008, India,Indain Institute of Tropical Meteorology, Pune-411008, India

Abstract: The impact of initial guess and grid resolutions on the analysis and prediction has been investigated over the In-dian region. For this purpose, an univariate objective analysis scheme and a primitive equation barotropic model have been used. The impact of initial guess and the resolutions on analysis and prediction is discussed.

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