How Much Skill Was There in Forecasting the Very Strong 1997–98 El Niño?
- 1 September 2000
- journal article
- Published by American Meteorological Society in Bulletin of the American Meteorological Society
- Vol. 81 (9) , 2107-2119
- https://doi.org/10.1175/1520-0477(2000)081<2107:hmswti>2.3.co;2
Abstract
The very strong 1997–98 El Niño was the first major event in which numerous forecasting groups participated in its real–time prediction. A previously developed simple statistical tool–the El Niño–Southern Oscillation Climatology and Persistence (ENSO–CLIPER) model–is utilized as a baseline for determination of skill in forecasting this event. Twelve statistical and dynamical models were available in real time for evaluation. Some of the models were able to outperform ENSO–CLIPER in predicting either the onset or the decay of the 1997–98 El Niño, but none were successful at both for a medium–range two season (6–8 months) lead time. There were no models, including ENSO–CLIPER, able to anticipate even one–half of the actual amplitude of the El Niño's peak at medium–range (6–11 months) lead. In addition, none of the models showed skill (i.e., lower root–mean–square error than ENSO–CLIPER) at the zero season (0–2 months) through the two season (6–8 months) lead times. No dynamical model and only two o... Abstract The very strong 1997–98 El Niño was the first major event in which numerous forecasting groups participated in its real–time prediction. A previously developed simple statistical tool–the El Niño–Southern Oscillation Climatology and Persistence (ENSO–CLIPER) model–is utilized as a baseline for determination of skill in forecasting this event. Twelve statistical and dynamical models were available in real time for evaluation. Some of the models were able to outperform ENSO–CLIPER in predicting either the onset or the decay of the 1997–98 El Niño, but none were successful at both for a medium–range two season (6–8 months) lead time. There were no models, including ENSO–CLIPER, able to anticipate even one–half of the actual amplitude of the El Niño's peak at medium–range (6–11 months) lead. In addition, none of the models showed skill (i.e., lower root–mean–square error than ENSO–CLIPER) at the zero season (0–2 months) through the two season (6–8 months) lead times. No dynamical model and only two o...Keywords
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