A New Method for Determining the Reliability of Dynamical ENSO Predictions

Determination of the reliability of particular ENSO forecasts is of particular importance to end users. Theoretical arguments are developed that indicate that the amplitudes of slowly decaying (or growing) normal modes of the coupled system provide a useful measure of forecast reliability. Historical forecasts from a skillful prediction model together with a series of ensemble predictions from a ‘‘perfect model’’ experiment are used to demonstrate that these arguments carry over to the practical prediction situation. In such a setting it is found that the amplitude of the dominant normal mode, which strongly resembles the observed ENSO cycle, is a potentially useful index of reliability. The fact that this index was generally lower in the 1970s than the 1980s provides an explanation for why many coupled models performed better in the latter decade. It does not, however, explain the low skill of some coupled models in the early 1990s as the index defined here was then moderate.

[1]  H. Storch,et al.  Principal oscillation patterns: a review , 1995 .

[2]  N. Smith,et al.  An Improved System for Tropical Ocean Subsurface Temperature Analyses , 1995 .

[3]  Andrew M. Moore,et al.  Stochastic forcing of ENSO by the intraseasonal oscillation , 1999 .

[4]  K. Hasselmann PIPs and POPs: The reduction of complex dynamical systems using principal interaction and oscillation patterns , 1988 .

[5]  F. Mélin,et al.  Role of Meridional Wind Anomalies in a Coupled Model of ENSO , 1996 .

[6]  M. Latif,et al.  Greenhouse Warming, Decadal Variability, or El Niño? An Attempt to Understand the Anomalous 1990s , 1997 .

[7]  Eugenia Kalnay,et al.  Ensemble Forecasting at NMC: The Generation of Perturbations , 1993 .

[8]  D. Battisti,et al.  Dynamics and Thermodynamics of a Warming Event in a Coupled Tropical Atmosphere–Ocean Model , 1988 .

[9]  Anthony C. Hirst,et al.  Interannual variability in a tropical atmosphere−ocean model: influence of the basic state, ocean geometry and nonlinearity , 1989 .

[10]  Prashant D. Sardeshmukh,et al.  The Optimal Growth of Tropical Sea Surface Temperature Anomalies , 1995 .

[11]  Richard Kleeman,et al.  Limits to predictability in a coupled ocean‐atmosphere model due to atmospheric noise , 1994 .

[12]  Jun-Ichi Yano,et al.  Time–Frequency Variability of ENSO and Stochastic Simulations , 1998 .

[13]  Mojib Latif,et al.  Predictability of a Stochastically Forced Hybrid Coupled Model of El Niño , 1997 .

[14]  M. Cane,et al.  On the prediction of ENSO: a study with a low-order Markov model , 1994 .

[15]  R. Kleeman On the Dependence of Hindcast Skill on Ocean Thermodynamics in a Coupled Ocean-Atmosphere Model , 1993 .

[16]  R. Kleeman,et al.  A recent change in the mean state of the Pacific basin climate: Observational evidence and atmospheric and oceanic responses , 1996 .

[17]  Cécile Penland,et al.  Prediction of Nino 3 sea surface temperatures using linear inverse modeling , 1993 .

[18]  Richard Kleeman,et al.  Skill assessment for ENSO using ensemble prediction , 1998 .

[19]  D. Gutzler,et al.  Estimating the Effect of Stochastic Wind Stress Forcing on ENSO Irregularity , 1997 .

[20]  David L. T. Anderson,et al.  Decadal and Seasonal Dependence of ENSO Prediction Skill , 1995 .

[21]  K. Wyrtki Fluctuations of the Dynamic Topography in the Pacific Ocean , 1975 .

[22]  A. Hirst Unstable and Damped Equatorial Modes in Simple Coupled Ocean-Atmosphere Models , 1986 .

[23]  C. J. Thompson Initial Conditions for Optimal Growth in a Coupled Ocean-Atmosphere Model of ENSO* , 1998 .

[24]  Mojib Latif,et al.  A review of the predictability and prediction of ENSO , 1998 .

[25]  Franco Molteni,et al.  Ensemble prediction using dynamically conditioned perturbations , 1993 .

[26]  Andrew M. Moore,et al.  A Theory for the Limitation of ENSO Predictability Due to Stochastic Atmospheric Transients , 1997 .

[27]  Dake Chen,et al.  An Improved Procedure for EI Ni�o Forecasting: Implications for Predictability , 1995, Science.

[28]  Neville Smith,et al.  Assimilation of Subsurface Thermal Data into a Simple Ocean Model for the Initialization of an Intermediate Tropical Coupled Ocean-Atmosphere Forecast Model , 1995 .

[29]  T. Palmer,et al.  Predictability of a Coupled Model of ENSO Using Singular Vector Analysis. Part II: Optimal Growth and Forecast Skill , 1997 .