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EXPERIMENTAL STUDY OF THE ROLE OF INITIAL AND BOUNDARY CONDITIONS IN MESOSCALE NUMERICAL WEATHER PREDICTION

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  • Based on the real case of a frontal precipitation process affecting South China, 27 controlled numerical experiments was made for the effects of hydrostatic and non-hydrostatic effects, different driving models, combinations of initial/boundary conditions, updates of lateral values and initial time levels of forecast, on model predictions. Features about the impact of initial/boundary conditions on mesoscale numerical weather prediction (NWP) model are analyzed and discussed in detail. Some theoretically and practically valuable conclusions are drawn. It is found that the overall tendency of mesoscale NWP models is governed by its driving model, with the initial conditions showing remarkable impacts on mesoscale models for the first I0 hours of the predictions while leaving lateral boundary conditions to take care the period beyond; the latter affect the inner area of mesoscale predictions mainly through the propagation and movement of weather signals (waves) of different time scales; initial values of external model parameters such as soil moisture content may affect predictions of more longer time validity, while fast signals may be filtered away and only information with time scale 4 times as large as or more than the updated period of boundary values may be introduced, through lateral boundary, to mesoseale models, etc. Some results may be taken as important guidance on mesoseale model and its data a.ssimilation developments of the future.
  • [1] CHEN De-hui, XUE Ji-shan, YANG Xue-sheng et al. Meteorological numerical forecasts in China facing the 21st century ― a summary report on the pre-study on the engineering system of innovative techniques of meteorological numerical forecasts in China facing the 21st century [C]. Beijing: Meteorological Press, 2001. 1-125.
    [2] STANIFORTH Andrew. Analysis on the impact of boundary information on inner area of the variational grid model, Workshop on limited area modeling [M]. Trieast, 1990.
    [3] GONG Jia-dong, Qiu Chong-jian, WANG Qiang et al. Numerical experiments on the assimilation of regional 4-dimension variance data [J]. Acta Meteorologica Sinica, 1999, 57(2): 131-142.
    [4] ZHANG Li-xiang, CHEN Li-qiang, ZHOU Xiao-shan et al. The verification and comparison of different initialization schemes in mesoscale numerical forecasts [J]. Meteorological Monthly, 2001, 27: 8-12.
    [5] CHEN De-hui, WANG Shi-wen, Numerical simulation and comparisons of initialization schemes for operational forecast [J]. Journal of Tropical Meteorology, 1996, 12: 356-364.
    [6] ZHOU Xia-qiong, DUAN Yi-hong, ZHU Yong-ti, The ensemble forecasting of tropical cyclone motion I:using a primitive equation barotropic model [J]. Journal of Tropical Meteorology, 2003, 19: 1-8.
    [7] YAN Jing-hua, Analysis of the performance of local elements forecast by the Guangzhou mesoscale model [J]. Quarterly Journal of Applied Meteorology, 2001. 12: 21-29.
    [8] D. Majewski,D. Liermann,P. Prohl,etal,The Operational Global Icosahedral-Hexagonal Gridpoint Model GME: Desvription and High-Resolution Tests[J]. Monthly Weather Reviews, 2002, 130: 319-338.
    [9] YAN Jing-hua, The South China regional short-term climate model and analysis of the performance [J]. Journal of Tropical Meteorology, 2000, 16(1): 9-17.
    [10] WANG Tie, ZHANG Li-feng, Experiment using nested models for medium-term numerical forecast [J]. Journal of Tropical Meteorology, 1997, 13 (4): 341-348.

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YAN Jing-hua, Detlev Majewski. EXPERIMENTAL STUDY OF THE ROLE OF INITIAL AND BOUNDARY CONDITIONS IN MESOSCALE NUMERICAL WEATHER PREDICTION [J]. Journal of Tropical Meteorology, 2003, 9(2): 134-142.
YAN Jing-hua, Detlev Majewski. EXPERIMENTAL STUDY OF THE ROLE OF INITIAL AND BOUNDARY CONDITIONS IN MESOSCALE NUMERICAL WEATHER PREDICTION [J]. Journal of Tropical Meteorology, 2003, 9(2): 134-142.
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EXPERIMENTAL STUDY OF THE ROLE OF INITIAL AND BOUNDARY CONDITIONS IN MESOSCALE NUMERICAL WEATHER PREDICTION

Abstract: Based on the real case of a frontal precipitation process affecting South China, 27 controlled numerical experiments was made for the effects of hydrostatic and non-hydrostatic effects, different driving models, combinations of initial/boundary conditions, updates of lateral values and initial time levels of forecast, on model predictions. Features about the impact of initial/boundary conditions on mesoscale numerical weather prediction (NWP) model are analyzed and discussed in detail. Some theoretically and practically valuable conclusions are drawn. It is found that the overall tendency of mesoscale NWP models is governed by its driving model, with the initial conditions showing remarkable impacts on mesoscale models for the first I0 hours of the predictions while leaving lateral boundary conditions to take care the period beyond; the latter affect the inner area of mesoscale predictions mainly through the propagation and movement of weather signals (waves) of different time scales; initial values of external model parameters such as soil moisture content may affect predictions of more longer time validity, while fast signals may be filtered away and only information with time scale 4 times as large as or more than the updated period of boundary values may be introduced, through lateral boundary, to mesoseale models, etc. Some results may be taken as important guidance on mesoseale model and its data a.ssimilation developments of the future.

YAN Jing-hua, Detlev Majewski. EXPERIMENTAL STUDY OF THE ROLE OF INITIAL AND BOUNDARY CONDITIONS IN MESOSCALE NUMERICAL WEATHER PREDICTION [J]. Journal of Tropical Meteorology, 2003, 9(2): 134-142.
Citation: YAN Jing-hua, Detlev Majewski. EXPERIMENTAL STUDY OF THE ROLE OF INITIAL AND BOUNDARY CONDITIONS IN MESOSCALE NUMERICAL WEATHER PREDICTION [J]. Journal of Tropical Meteorology, 2003, 9(2): 134-142.
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