Zheng Bin, Li Chunhui, Lin Ailan, et al. Prediction experiment for the South China Sea summer monsoon strength by physical-statistic integrated model. J Appl Meteor Sci, 2017, 28(5): 579-588. DOI:  10.11898/1001-7313.20170506.
Citation: Zheng Bin, Li Chunhui, Lin Ailan, et al. Prediction experiment for the South China Sea summer monsoon strength by physical-statistic integrated model. J Appl Meteor Sci, 2017, 28(5): 579-588. DOI:  10.11898/1001-7313.20170506.

Prediction Experiment for the South China Sea Summer Monsoon Strength by Physical-statistic Integrated Model

DOI: 10.11898/1001-7313.20170506
  • Received Date: 2017-01-09
  • Rev Recd Date: 2017-06-19
  • Publish Date: 2017-09-30
  • The South China Sea summer monsoon (SCSSM) is a tropical system that plays a key role during the flood season of South China. However, the prediction of the SCSSM strength is difficult by no matter dynamic or statistic methods. Statistic methods are used in practice rather than dynamic model, but empirical-statistic models always have good hindcasting results during the period of building model, while the forecasting skills decrease evidently in practice. Physical-statistic methods have relatively stable predictive skill when the persistence of physical processes is taken into account. Therefore, an integrated technique is introduced based on associated physical processes to establish a predictive model for SCSSM. It is well known that the rainfall of SCSSM has multi-scale climate variability, for example, quasi-biennial and quasi-quadrennial time scale, which are mainly related to TBO (Tropospheric Biennial Oscillation) and ENSO (El Niño-Southern Oscillation), respectively. Based on the corresponding climatic factors, a physical-statistic integrated model is built. Combined with the traditional empirical-statistic method, a new prediction model (namely physical and empirical-statistic integrated model) for SCSSM is developed.First, original data are processed by removing the climatic state (1981-2010) and linear trend, and then anomalous data are filtered on the TBO (12-36 months) and ENSO (36-96 months) time scales since the biennial mode of SCSSM has little connection with the ENSO. Second, regressed results based on climatic factors (e.g., sea surface temperature anomalies in Niño3.4 and the tropical western Pacific, precipitation anomalies over the maritime continent and Australian monsoon region) are assembled according to a discrimination function that is correlation coefficient larger than 0.05 significant level between regressed results and the filtered SCSSM precipitation. Moreover, the rest precipitation with SCSSM inter-annual variations removed is predicted by the traditional empirical-statistic method and results are added to those by the physical-statistic integrated model. Using data throughout 1979-2010, the physical and empirical-statistic integrated model is trained and results of 2011-2016 are predicted for test, compared with that of the empirical-statistic integrated model. It shows that the new model has better prediction skill (9.5% improvements in prediction score and 75% in anomaly correlation coefficient) and relatively stable predicting results. More than that, the new model has some predictive ability for SCSSM rainfall distribution.
  • Fig. 1  Air-sea interactive physical processes related with the Tropospheric Biennial Oscillation of the South China Sea summer monsoon (SCSSM)

    Fig. 2  Summer precipitation anomaly percentages of the observed and the predictand over the South China Sea during 2011-2016

    Fig. 3  The predicted summer precipitation anomaly percentage over the South China Sea during 2012

    (a)non-interannual component from empirical-statistic integrated model, (b)interannual component from physical-statistic integrated model

    Fig. 4  The South China Sea summer precipitation in 2011-2016

    (a)area correlation coefficients of summer precipitation anomaly and interannual component(12-96 months), (b)mean amplitude ratios(regional mean ratio of interannual variance to total one), (c)ACC test of predicted precipitation by PHEMS-INT model

    Table  1  Predictive factors for the physical-statistic SCSSM predictive model

    季节 准两年模态 4~5年模态
    海洋大陆 热带西太平洋 澳大利亚季风区 Niño3.4区 西北太平洋 南海季风区
    冬季
    (12月—次年2月)
    海温异常 降水异常 海温异常 海温异常 海温异常
    春季
    (3—5月)
    海温异常
    降水异常
    海温变率 海温异常 海温异常
    DownLoad: Download CSV

    Table  2  Comparison of SCSSM predictive models

    检验方法 1982—2010年回报试验 2011—2016年独立样本检验
    集成经验统计模型 集成物理-经验统计模型 集成经验统计模型 集成物理-经验统计模型
    PS 90.72 79.63 74.27 81.3
    ACC 0.75 0.40 0.28 0.49
    DownLoad: Download CSV
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    • Received : 2017-01-09
    • Accepted : 2017-06-19
    • Published : 2017-09-30

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