A novel approach to improve numerical weather prediction skills by using anomaly integration and historical data

[1] Using the concept of anomaly integration and historical climate data, we have developed a novel operational framework to implement deterministic numerical weather prediction within 15 days. Real-case validation shows pronounced improvements in the forecasts of global geopotential heights in 20 out of 30 cases with the Community Atmosphere Model version 3.0. Seven other cases are marginally improved, and only three are deteriorated, in which all are ameliorated within the first-week period. The average of the 30 cases shows an obvious increase of anomaly correlation coefficient (ACC) and a decrease of root mean square error (RMSE) of the geopotential height over global, hemispherical, and tropical zones. Significant amelioration on tropical circulation is displayed within the first-week prediction. The forecasting skill is extended by 0.6 day in terms of days of the ACC greater than 0.6 for 500 hPa 30 case averaged geopotential height on global scale. The 30 case mean ACC and RMSE of 500 hPa temperature show the increment of 0.2 and −1.6 K, respectively, in the first-week prediction. In the case of January 2008, much more reasonable horizontal distribution and vertical structure are achieved in bias-corrected model geopotential height, temperature, relative humidity, and horizontal wind components in comparison to reanalysis data. In spite of a need for additional storage of historical modeling data, the new method does not increase computational costs and therefore is suitable for routine application.

[1]  Alberto Arribas,et al.  The GloSea4 Ensemble Prediction System for Seasonal Forecasting , 2011 .

[2]  B. Briegleb Delta‐Eddington approximation for solar radiation in the NCAR community climate model , 1992 .

[3]  Heating and Kinetic Energy Dissipation in the NCAR Community Atmosphere Model , 2003 .

[4]  R. Dickinson,et al.  The land surface climatology of the community land model coupled to the NCAR community climate model , 2002 .

[5]  Changzhu Li,et al.  The Great 2008 Chinese Ice Storm: Its Socioeconomic–Ecological Impact and Sustainability Lessons Learned , 2011 .

[6]  G. Kauffman,et al.  The NCAR CSM Flux Coupler , 1996 .

[7]  G. Holland,et al.  Model Investigations of the Effects of Climate Variability and Change on Future Gulf of Mexico Tropical Cyclone Activity , 2010 .

[8]  J. Chao,et al.  長期数値予報の理論と方法;長期数値予報の理論と方法;A Theory and Method of Long-Range Numerical Weather Forecasts , 1982 .

[9]  P. Houtekamer,et al.  Data Assimilation Using an Ensemble Kalman Filter Technique , 1998 .

[10]  Zong‐Liang Yang,et al.  An Improved Dynamical Downscaling Method with GCM Bias Corrections and Its Validation with 30 Years of Climate Simulations , 2012 .

[11]  Andrew C. Lorenc,et al.  Analysis methods for numerical weather prediction , 1986 .

[12]  Adam A. Scaife,et al.  Atmospheric Blocking and Mean Biases in Climate Models , 2010 .

[13]  Veerabhadran Ramanathan,et al.  A nonisothermal emissivity and absorptivity formulation for water vapor , 1986 .

[14]  Wang Shaowu,et al.  An analogue‐dynamical long‐range numerical weather prediction system incorporating historical evolution , 1993 .

[15]  N. McFarlane,et al.  Sensitivity of Climate Simulations to the Parameterization of Cumulus Convection in the Canadian Climate Centre General Circulation Model , 1995, Data, Models and Analysis.

[16]  G. Dimego,et al.  The National Meteorological Center Regional Analysis System , 1988 .

[17]  J. Slingo The Development and Verification of A Cloud Prediction Scheme For the Ecmwf Model , 2007 .

[18]  K. Miyakoda,et al.  Essay on Dynamical Long-Range Forecasts of Atmospheric Circulation , 1982 .