Tang Shengjun, Wang Donghai, Du Jun, et al. The experiment of hybrid ensemble forecast approach in short-range forecast for South China rainstorm. J Appl Meteor Sci, 2015, 26(6): 669-679. DOI:  10.11898/1001-7313.20150603.
Citation: Tang Shengjun, Wang Donghai, Du Jun, et al. The experiment of hybrid ensemble forecast approach in short-range forecast for South China rainstorm. J Appl Meteor Sci, 2015, 26(6): 669-679. DOI:  10.11898/1001-7313.20150603.

The Experiment of Hybrid Ensemble Forecast Approach in Short-range Forecast for South China Rainstorm

DOI: 10.11898/1001-7313.20150603
  • Received Date: 2015-03-25
  • Rev Recd Date: 2015-06-10
  • Publish Date: 2015-11-30
  • Hybrid ensemble forecast approach composed of high-resolution and low-resolution model is tested with multi-initial conditions and multi-physics ensemble prediction system (EPS) based on ARPS and WRF. Three kinds of ensemble prediction experiments (ARPS model ensemble, WRF model ensemble and ARPS-WRF multi-model ensemble) are designed to comparatively analyze the precipitation effect between the hybrid ensemble forecast approach and traditional ensemble forecast approach based on the heavy rainfall event occurred in Southern China on 8 May 2013. ARPS model ensemble improves local precipitation simulation over southern part of Guangdong Province. The center intensity of southern ensemble mean reaches 150 mm, close to the observation, but its location shifts northeast a little. The distribution of ensemble spread is similar to that of ensemble mean. The probabilistic forecast area of the approach is close to the observation in terms of the torrential rain and downpour forecast. The Threat Score (TS) show that the greatest improvements for order of magnitude precipitation are obtained by the hybrid ensemble approach. The Brier Score (BS) also shows that the improvement on moderate rain, heavy rain and torrential rain is obvious, but the improvement on downpour and excessive storm is limited for the approach. WRF model ensemble has a better performance on precipitation simulation over northern part of Guangdong Province, but the hybrid approach is limited because of the large frequency of false alarms and misses. ARPS-WRF multi-models obviously improve precipitation simulation which has a better performance than those of traditional ensemble forecast approach on precipitation area and intensity. The center intensity of southern precipitation reaches 70 mm, less than the observation and it is caused by the weaker WRF members forecast. The distribution of ensemble spread is similar to that of ensemble mean. The probabilistic forecast of torrential rain and downpour in southern area is best up to 40%. The TS shows that the greatest improvements for order of magnitude precipitation are obtained by the hybrid ensemble approach, especially for heavy rain, torrential rain and downpour. The BS also shows that the improvement on moderate rain, heavy rain and torrential rain is obvious. ARPS-WRF multi-models have better performance than ARPS model on the forecast of downpour and excessive storm. Therefore, the hybrid ensemble forecast approach achieves high-resolution ensemble forecast system and improves the precipitation simulation combining low-resolution ensemble run with single high-resolution control model run. Meanwhile, a reference to high-resolution ensemble forecast system is provided for operational weather prediction centers.
  • Fig. 1  Observed precipitation from 0800 BT to 2000 BT on 8 May 2013

    Fig. 2  12 h accumulative precipitation ensemble mean and spread of 3 schemes in ARPS

    Fig. 3  12 h precipitation probabilistic forecast of 3 schemes in ARPS

    Fig. 4  Threat Score and Brier Score of 12 h accumulative precipitation for 3 schemes in ARPS

    Fig. 5  12 h accumulative precipition ensemble mean and spread of 3 schemes in WRF

    Fig. 6  Threat Score and Brier Score of 12 h accumulative precipitation for 3 schemes in WRF

    Fig. 7  12 h accumulative precipitation ensemble mean and spread of 3 schemes in ARPS-WRF

    Fig. 8  12 h precipitation probabilistic forecast of 3 schemes in ARPS-WRF

    Fig. 9  Threat Score and Brier Score of 12 h accumulative precipitation for 3 schemes in ARPS-WRF

    Table  1  The formation of ensemble members of the system

    成员 微物理方案 积云对流方案 边界层方案
    ARPS_ctl LIN KF PBL specified
    ARPS_n1 WARMRA Kuo+Kessler PBL diagnosed
    ARPS_p1 WARMRA KF PBL diagnosed
    ARPS_n2 NEMICE KF PBL specified
    ARPS_p2 LIN New KF PBL diagnosed
    ARPS_n3 NEMICE Kuo+Kessler PBL diagnosed
    ARPS_p3 WARMRA New KF PBL specified
    WRF_ctl LIN BMJ MYJ
    WRF_n1 LIN New KF MYJ
    WRF_p1 Thompson BMJ YSU
    WRF_n2 WSM6 BMJ YSU
    WRF_p2 WSM5 New KF MYJ
    WRF_n3 Ferrier New KF YSU
    WRF_p3 WSM5 BMJ MYJ
    注:n代表负扰动成员,p代表正扰动成员,ctl代表控制预报。
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    • Received : 2015-03-25
    • Accepted : 2015-06-10
    • Published : 2015-11-30

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