欢迎访问中国科学院大学学报,今天是
优秀博士论文

一个新的大样本ENSO集合预报系统的发展与检验

  • 郑飞 ,
  • 朱江
展开
  • 中国科学院大气物理研究所,北京 100029
郑飞:获2008年度中国科学院优秀博士学位论文奖和2009年度全国百篇优秀博士学位论文奖. 现主要从事短期气候预测、集合资料同化与集合预报研究.
导师 朱江 研究员:主要研究领域为资料同化的方法以及在海洋、大气和环境中的应用.

收稿日期: 2009-12-08

  网络出版日期: 2010-05-15

基金资助

Supported by the Natural Science Foundation of China (40805033), the Chinese Academy of Science (KZCX2-YW-202), the Chinese COPES Project (GYHY-200706005), and the National Basic Research Program of China (2006CB403600) 

Developments and verifications of a new large size ENSO ensemble prediction system

  • ZHENG Fei ,
  • ZHU Jiang
Expand
  • Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China

Received date: 2009-12-08

  Online published: 2010-05-15

Supported by

Supported by the Natural Science Foundation of China (40805033), the Chinese Academy of Science (KZCX2-YW-202), the Chinese COPES Project (GYHY-200706005), and the National Basic Research Program of China (2006CB403600) 

摘要

详细介绍了一个新的大样本集合预报系统. 为了减小ENSO(厄尔尼诺-南方涛动)预报中的预报不确定性,该集合预报系统首先基于一个中等复杂程度的耦合模式,利用集合卡尔曼滤波资料同化方法同化有效的海洋观测资料为集合预报系统提供集合初始场;同时,一个发展的用于12个月预报的一阶线性马尔可夫(Markov)随机误差模式被嵌套到集合预报系统中来模拟模式不确定性. 基于1992年11月~2008年10月100个样本的集合回报试验,从确定性预报技巧和概率预报技巧2个方面对集合预报系统的预报水平进行了检验. 该集合预报方法能够很有效地将传统的确定性预报扩展到概率预报领域,且检验结果表明,预报样本均值的预报水平要优于单一的确定性预报. 对于概率预报而言,集合预报样本能够很好地跟随观测的变化,并且能够提供单纯确定性预报所不能够提供的额外信息.

本文引用格式

郑飞 , 朱江 . 一个新的大样本ENSO集合预报系统的发展与检验[J]. 中国科学院大学学报, 2010 , 27(3) : 420 -431 . DOI: 10.7523/j.issn.2095-6134.2010.3.017

Abstract

A new large size ensemble prediction system (EPS) is introduced in this paper. To minimize the forecast uncertainties for ENSO (El Ni o-Southern Oscillation) predictions, the EPS is firstly based on an intermediated coupled model (ICM), and then the ensemble Kalman filter (EnKF) data assimilation method is adopted to generate the initial ensemble conditions for the EPS through assimilating available oceanic observations. Meanwhile, a developed linear, first-order Markov stochastic model-error model is embedded in the EPS to represent the model uncertainties during the twelve-month ensemble forecast process. The prediction skill of the EPS is verified based on the (100-members) retrospective ensemble forecast experiment covering the period between November, 1992 and October, 2008 in both deterministic and probabilistic senses. This ensemble technique provides a successful method of extending the standard deterministic forecasts to the probabilistic domain. The verification results show that the prediction skill of the ensemble mean is better than that of one single deterministic forecast using the same ICM. For the probabilistic perspective, those ensemble forecasts have their ensembles following observational variations well, and provide additional information that could not be gleaned from a purely deterministic approach.

参考文献


[1] Wang C, Picaut J. Understanding ENSO physics—A review. Earth Climate: the ocean-atmosphere interaction
[J]. Geophys Monogr Amer Geophys Union, 2004, 147: 21- 48.

[2] Jin E K, James L K, Wang B, et al. Current status of ENSO prediction skill in coupled ocean-atmosphere models
[J]. Climate Dyn, 2008, 31: 647-664.

[3] Kirtman P B. The COLA anomaly coupled model: ensemble ENSO prediction
[J]. Mon Wea Rev, 2003, 131: 2324-2341.

[4] Chen D, Cane M A. El Nino prediction and predictability
[J]. J of Computational Physics, 2008, 227: 3625-3640.

[5] Palmer T N. Predicting uncertainty in forecasts of weather and climate
[J]. Rep Prog Phys, 2000, 63: 71-116.

[6] Moore A M, Kleeman R. Skill assessment for ENSO using ensemble prediction
[J]. Quart J Roy Meteor Soc, 1998, 124: 557-584.

[7] Kleeman R, Moore A M. A new method for determining the reliability of dynamical ENSO predictions
[J]. Mon Wea Rev, 1999, 127: 694-705.

[8] DeWitt D G. Retrospective forecasts of interannual sea surface temperature anomalies from 1982 to present using a directly coupled atmosphere-ocean general circulation model
[J]. Mon Wea Rev, 2005, 133: 2972-2995.

[9] Mitchell H L, Houtekamer P L, Pellerin G. Ensemble size, balance, and model-error representation in an ensemble Kalman filter
[J]. Mon Wea Rev, 2002, 130: 2791-2808.

[10] Zheng F, Zhu J, Zhang R H, et al. Ensemble hindcasts of SST anomalies in the tropical Pacific using an intermediate coupled model
[J]. Geophys Res Lett, 2006, 33: L19604. doi: 10.1029/2006GL026994.

[11] Zheng F, Zhu J, Zhang R H. Impact of altimetry data on ENSO ensemble initializations and predictions
[J]. Geophys Res Lett, 2007, 34: L13611. doi: 10.1029/2007GL030451.

[12] Zheng F. Researches on ENSO ensemble predictions . Beijing: Institute of Atmospheric Physics, Chinese Academy of Sciences, 2007.

[13] Evensen G. The ensemble Kalman filter: theoretical formulation and practical implementation
[J]. Ocean Dyn, 2003, 53: 343-367.

[14] Evensen G. Sampling strategies and square root analysis schemes for the EnKF
[J]. Ocean Dyn, 2004, 54: 539-560.

[15] Zheng F, Zhu J. Balanced multivariate model errors of an intermediate coupled model for ensemble Kalman filter data assimilation
[J]. J Geophys Res, 2008, 113: C07002. doi:10.1029/2007JC004621.

[16] Zheng F, Zhu J, Wang H, et al. Ensemble hindcasts of ENSO events over the past 120 years using a large number of ensembles
[J]. Adv Atmos Sci, 2009, 26: 359-372.

[17] Zheng F, Wang H, Zhu J. ENSO ensemble prediction: initial condition perturbations vs. model perturbations
[J]. Chin Sci Bull, 2009, 54: 2516-2523.

[18] Keenlyside N, Kleeman R. On the annual cycle of the zonal currents in the equatorial Pacific
[J]. J Geophys Res, 2002, 107: doi:10.1029/2000JC0007111.

[19] Zhang R H, Zebiak S E, Kleeman R, et al. A new intermediate coupled model for El Ni o simulation and prediction
[J]. Geophys Res Lett, 2003, 30: 2012. doi:10.1029/2003GL018010.

[20] McCreary J P. A linear stratified ocean model of the equatorial undercurrent
[J]. Philosophical Transactions of the Royal Society (London), 1981, 298: 603-635.

[21] Zhang R H, Zebiak S E, Kleeman R, et al. Retrospective El Ni o forecast using an improved intermediate coupled model
[J]. Mon Wea Rev, 2005, 133: 2777-2802.

[22] Smith T M, Reynolds R W, Peterson T C, et al. Improvements to NOAAs historical merged land-ocean surface temperature analysis (1880-2006) . J Climate, 2008, 21: 2283-2296.

[23] Lagerloef G S E, Mitchum G, Lukas R, et al. Tropical Pacific near-surface currents estimated from altimeter, wind, and drifter data
[J]. J Geophys Res, 1999, 104: 23313-23326.

[24] Leith C E. Theoretical skill of Monte Carlo forecasts
[J]. Mon Wea Rev, 1974, 102: 409-418.

[25] Toth Z, Kalnay E. Ensemble forecasting at NCEP and the breeding method
[J]. Mon Wea Rev, 1997, 125: 3297-3319.

[26] Talagrand O, Vautard R, Strauss B. Evaluation of probabilistic prediction systems //Proceedings, ECMWF Workshop on Predictability, 1997.

[27] Hamill T M. Interpretation of rank histograms for verifying ensemble forecasts
[J]. Mon Wea Rev, 2001, 129: 550-560.

[28] Mason S J, Graham N E. Conditional probabilities, relative operating characteristics, and relative operating levels
[J]. Wea Forecasting, 1999, 14: 713-725.

[29] Balmaseda M A, Davey M K, Anderson D L T. Decadal and seasonal dependence of ENSO prediction skill
[J]. J Climate, 1995, 8: 2705-2715.

文章导航

/