留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

区域集合预报系统2 m温度预报的校准技术

王敏 李晓莉 范广洲 李泽椿

王敏, 李晓莉, 范广洲, 等. 区域集合预报系统2 m温度预报的校准技术. 应用气象学报, 2012, 23(4): 395-401..
引用本文: 王敏, 李晓莉, 范广洲, 等. 区域集合预报系统2 m温度预报的校准技术. 应用气象学报, 2012, 23(4): 395-401.
Wang Min, Li Xiaoli, Fan Guangzhou, et al. Calibrating 2 m temperature forecast for the regional ensemble prediction system at NMC. J Appl Meteor Sci, 2012, 23(4): 395-401.
Citation: Wang Min, Li Xiaoli, Fan Guangzhou, et al. Calibrating 2 m temperature forecast for the regional ensemble prediction system at NMC. J Appl Meteor Sci, 2012, 23(4): 395-401.

区域集合预报系统2 m温度预报的校准技术

资助项目: 

公益性行业 (气象) 科研专项 GYHY201006015

详细信息
    通信作者:

    李晓莉, E-mail: lixl@cma.gov.cn

Calibrating 2 m Temperature Forecast for the Regional Ensemble Prediction System at NMC

  • 摘要: 采用非齐次高斯回归 (NGR) 技术对国家气象中心区域集合预报系统的2 m温度预报结果开展了一阶偏差和二阶离散度的校准研究。对预报结果比较详尽的检验分析表明:校准后的2 m温度预报可靠性和预报技巧均显著提高,表现为校准后集合预报成员的均方根误差与离散度更为接近;原Talagrand直方图中的“L”形分布现象得到有效改善;Brier评分、最小连续分级概率评分 (CRPS) 明显减小,相对作用特征 (ROC) 面积增大,说明校准后的2 m温度预报表现出更好的预报技能。此外,NGR技术与自适应误差订正技术的对比试验表明,NGR在消除集合平均偏差和提高集合离散度两个方面均有优势。
  • 图  1  2008年7月20日12:00起报的2 m温度集合平均 (预报时效为30 h) 与观测场之差的空间分布

    (a) 校准前,(b) 校准后

    Fig. 1  Distribution of the difference of 30-hour 2 m temperation forecast at 1200 UTC 20 July 2008

    (a) the difference between ensemble averge of model direct output and observation, (b) the difference between calibrated ensemble average and observation

    图  2  2 m温度预报的均方根误差和离散度

    Fig. 2  RMSE and ensemble spread of 2 m temperature

    图  3  2 m温度预报Talagrand分布

    Fig. 3  Talagrand diagrams of raw and calibrated 2 m temperature (forecast lead time is 6 hours)

    图  4  2 m温度预报BS评分

    Fig. 4  BS of raw and calibrated 2 m temperature

    图  5  2 m温度预报CRPS评分

    Fig. 5  CRPS of raw and calibrated 2 m temperature

    图  6  2 m温度预报ROC面积

    Fig. 6  Area under ROC curves for 2 m temperature

    图  7  不同训练期的2 m温度预报CRPS评分

    Fig. 7  CRPS of 2 m temperature from different training length

    图  8  不同离散度因子的2 m温度预报CRPS评分

    Fig. 8  CRPS of 2 m temperature from different spread rescaling

    图  9  2 m温度预报的均方根误差

    Fig. 9  RMSE of 2 m temperature

    图  10  2 m温度预报的BS评分

    Fig. 10  BS of 2 m temperature

    图  11  2 m温度预报的CRPS评分

    Fig. 11  CRPS of 2 m temperature

    图  12  2 m温度预报ROC面积

    Fig. 12  Area under ROC curves for 2 m temperature

  • [1] Carter G M, Dallavalle J P, Glahn H R. Statistical forecasts based on the National Meteorological Center's numerical weather prediction system. Wea Forecasting, 1989, 4: 401-412. doi:  10.1175/1520-0434(1989)004<0401:SFBOTN>2.0.CO;2
    [2] Vislocky R L, Fritsch J M. Performance of an advanced MOS system in the 1996-97 national collegiate weather forecasting contest. Bull Amer Meteor Soc, 1997, 78:2851-2857. doi:  10.1175/1520-0477(1997)078<2851:POAAMS>2.0.CO;2
    [3] Raftery A E, Gneiting T, Balabdaoui F, et al. Using Bayesian model averaging to calibrate forecast ensembles. Mon Wea Rev, 2005, 133:1155-1174. doi:  10.1175/MWR2906.1
    [4] Gneiting T, Raftery A E, Westveld A H, et al. Calibrated probabilistic forecasting using ensemble model output statistics and minimum CRPS estimation. Mon Wea Rev, 2005, 133:1098-1118. doi:  10.1175/MWR2904.1
    [5] Hamill T M, Whitaker J S, Wei X. Ensemble reforecasting: Improving medium range forecast skill using retro-spective forecasts. Mon Wea Rev, 2004, 132:1434-1447. doi:  10.1175/1520-0493(2004)132<1434:ERIMFS>2.0.CO;2
    [6] Hamill T M, Whitaker J S. Probabilistic quantitative precipitation forecasts based on reforecast analogs: Theory and application. Mon Wea Rev, 2006, 134: 3209-3229. doi:  10.1175/MWR3237.1
    [7] Hamill T M, Whitaker J S. Ensemble calibration of 500-hPa geopotential height and 850-hPa and 2-m temperatures using reforecasts. Mon Wea Rev, 2007, 135:3273-3280. doi:  10.1175/MWR3468.1
    [8] Hamill T M, Whitaker J S, Mullen S L. Reforecasts: An important dataset for improving weather predictions. Bull Amer Meteor Soc, 2006, 87:33-46. doi:  10.1175/BAMS-87-1-33
    [9] Cui B, Toth Z, Zhu Y, et al. The Trade-off in Bias Correction Between Using the Latest Analysis/Modeling System with a Short, Versus an Older System with a Long Archive. Proc First THORPEX Int Science Symp, Montreal, Canada, World Meteorological Organization, 2006:281-284.
    [10] 林春泽, 智协飞, 韩艳, 等.基于TIGGE资料的地面气温多模式超级集合预报研究.应用气象学报, 2009, 20(6):706-712. doi:  10.11898/1001-7313.20090608
    [11] 马清, 龚建东, 李莉, 等.超级集合预报的误差订正与集成研究.气象, 2008, 34(3):42-48. doi:  10.7519/j.issn.1000-0526.2008.03.007
    [12] Kunii M, Saito K, Seko H, et al. Verifications and intercomparisons of mesoscale ensemble prediction systems in B08RDP. Tellus, 2011, 63A: 531-549. doi:  10.1088/1742-6596/454/1/012073/pdf
    [13] Alexander Kann, Wittmann Christpoh, Wang Yong. Calibrating 2 m temperature of limmited-area ensember forecasts using high-resolution analysis. Mon Wea Rew, 2009, 137:3373-3387. doi:  10.1175/2009MWR2793.1
    [14] 邓国, 龚建东, 邓莲堂, 等.国家级区域集合预报系统研发和性能检验.应用气象学报, 2010, 21(5):513-523. doi:  10.11898/1001-7313.20100501
    [15] Nelder J A, Mead R. A simplex method for function minimization. Comput J, 1965, 7:308-313. doi:  10.1093/comjnl/7.4.308
    [16] Hagedorn R, Hamill T M, Whitaker J S. Probabilistic forecast calibration using ECMWF and GFS ensemble reforecasts. Part Ⅰ: Temperature. Mon Wea Rev, 2008, 136: 2608-2619. doi:  10.1175/2007MWR2410.1
    [17] 皇甫雪官.国家气象中心集合数值预报检验评价.应用气象学报, 2002, 13(1):29-36. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20020103&flag=1
  • 加载中
图(12)
计量
  • 摘要浏览量:  4093
  • HTML全文浏览量:  1092
  • PDF下载量:  1612
  • 被引次数: 0
出版历程
  • 收稿日期:  2011-08-05
  • 修回日期:  2012-05-10
  • 刊出日期:  2012-08-31

目录

    /

    返回文章
    返回