Dong Xiaoyun, Yu Jinhua, Liang Xinzhong, et al. Bias correction of summer extreme precipitation simulated by CWRF model. J Appl Meteor Sci, 2020, 31(4): 504-512. DOI:  10.11898/1001-7313.20200412.
Citation: Dong Xiaoyun, Yu Jinhua, Liang Xinzhong, et al. Bias correction of summer extreme precipitation simulated by CWRF model. J Appl Meteor Sci, 2020, 31(4): 504-512. DOI:  10.11898/1001-7313.20200412.

Bias Correction of Summer Extreme Precipitation Simulated by CWRF Model

DOI: 10.11898/1001-7313.20200412
  • Received Date: 2020-02-05
  • Rev Recd Date: 2020-04-28
  • Publish Date: 2020-07-31
  • The accurate forecast of extreme precipitation plays an important role in guiding the national economy and people's livelihood. The newly developed Climate-Weather Research and Forecasting model (CWRF) integrates a comprehensive ensemble of alterable parameterization schemes for each of the key physical processes, including surface (land, ocean), planetary boundary layer, cumulus (deep, shallow), microphysics, cloud, aerosol, and radiation. This facilitates the use of an optimized physics ensemble approach to improve weather and climate prediction. Evaluating the simulation performance and correcting the error can effectively improve the operational prediction level of extreme precipitation in CWRF model.Daily rainfall data simulated by CWRF model and observed at 2416 meteorological stations in China from June to August during 1980-2015 are used to compare correcting effects of Q-lin, Q-tri, RQ-lin, RQ-tri, SSP-lin and CDFt on extreme precipitation of control scheme simulated by CWRF in eastern China. Based on the simulation performance ranking of 14 parameterization schemes in CWRF model, effects of the top 4, the latter 4 and the ensemble of 14 parameterization schemes are compared. Correcting effects of two approaches are compared: Revising after the collection of members and revising before the collection of members. Main results show that the error of the extreme precipitation simulation of C1 scheme can be obviously reduced by using six error correction methods, among which the RQ-lin correction method is the best. Although there are great differences between parameterization schemes in the simulation of extreme precipitation index, CWRF model shows good ability for extreme precipitation index in eastern China. The first four parametric schemes with good extreme precipitation simulation ability are C13, C14, C12 and C1, while the C6, C4, C3 and C10 schemes perform worse, respectively. Different parameterization schemes are revised to ensure that it is the closest to the average value of observed extreme precipitation after each of 14 members of the parameterization scheme being revised. Results have important application value for improving outputs of model and improving its prediction ability.Error correction can only be used as a supplementary means to improve extreme precipitation prediction. The precision of model physical process and the improvement of model resolution are the key to improve extreme precipitation prediction.
  • Fig. 1  Daily extreme precipitation from observation and simulation by CWRF control scheme(C1) with its revision under 6 methods in validation period

    Fig. 2  Taylor score for 5 simulated extreme indices of 14 parameterization schemes of CWRF Model

    Fig. 3  M2 for 5 simulated extreme indices of 14 parameterization schemes of CWRF Model

    Fig. 4  Daily extreme precipitation mean for different parameterization schemes under RQ-lin revision and observation (a)observation, (b)C1, (c)sets of C1, C12, C13 and C14, (d)sets of C3, C4, C6 and C10, (e)sets of C1-C14

    Fig. 5  Daily extreme precipitation mean of 14 parameterization schemes revised and regrouped

    Table  1  Parameterization schemes of CWRF

    方案积云对流参数化微物理过程参数化
    C1ECP & UWGSFCGCE
    C2KFetaGSFCGCE
    C3BMJGSFCGCE
    C4GrellGSFCGCE
    C5NSASGSFCGCE
    C6DonnerGSFCGCE
    C7EmanuelGSFCGCE
    C8ECP & UWLin
    C9ECP & UWWSM6
    C10ECP & UWEtamp-new
    C11ECP & UWThompson
    C12ECP & UWThompson-aero
    C13ECP & UWMorrison
    C14ECP & UWMorrison-aerosol
    DownLoad: Download CSV

    Table  2  Extreme rainfall indices

    指数名称缩写定义单位
    降水强度SDII总降水量/有雨日数mm·d-1
    暴雨日数R50日降水量不低于50 mm的日数d
    第95百分位降水量P95日降水量在第95百分位的值mm
    强降水量R95P日降水量大于第95百分位值的总降水量mm
    极端降水贡献率R95T超过第95百分位降水量之和占总降水量的百分率%
    DownLoad: Download CSV

    Table  3  Regional correlation coefficient and root mean square error of daily extreme precipitation mean from observation to revision of CWRF control scheme(C1) under 6 methods in validation period

    订正方法相关系数均方根误差
    Q-lin0.8110.29
    Q-tri0.7811.64
    RQ-lin0.8210.03
    RQ-tri0.8010.75
    SSP-lin0.6718.76
    CDFt0.7315.77
    DownLoad: Download CSV

    Table  4  Ranking of simulation capabilities of 14 parameterization schemes

    方案泰勒评分时间变率综合
    C1384
    C2845
    C3101312
    C4141113
    C51128
    C6131414
    C712710
    C8588
    C9485
    C1091111
    C11665
    C12643
    C13111
    C14222
    DownLoad: Download CSV
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    • Received : 2020-02-05
    • Accepted : 2020-04-28
    • Published : 2020-07-31

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