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Extended-range statistical ENSO prediction through operator-theoretic techniques for nonlinear dynamics

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arxiv 1906.09492 v3 pith:PMRHUVLJ submitted 2019-06-22 physics.ao-ph physics.data-an

Extended-range statistical ENSO prediction through operator-theoretic techniques for nonlinear dynamics

classification physics.ao-ph physics.data-an
keywords ensodynamicsmodelsforecastingmonthsnonlinearstatisticalanalog
verification ladder T0 review T1 audit T2 compute T3 formal T4 reserved
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Forecasting the El Nino-Southern Oscillation (ENSO) has been a subject of vigorous research due to the important role of the phenomenon in climate dynamics and its worldwide socioeconomic impacts. Over the past decades, numerous models for ENSO prediction have been developed, among which statistical models approximating ENSO evolution by linear dynamics have received significant attention owing to their simplicity and comparable forecast skill to first-principles models at short lead times. Yet, due to highly nonlinear and chaotic dynamics (particularly during ENSO initiation), such models have limited skill for longer-term forecasts beyond half a year. To resolve this limitation, here we employ a new nonparametric statistical approach based on analog forecasting, called kernel analog forecasting (KAF), which avoids assumptions on the underlying dynamics through the use of for nonlinear kernel methods for machine learning and dimension reduction of high-dimensional datasets. Through a rigorous connection with Koopman operator theory for dynamical systems, KAF yields statistically optimal predictions of future ENSO states as conditional expectations, given noisy and potentially incomplete data at forecast initialization. Here, using industrial-era Indo-Pacific sea surface temperature (SST) as training data, the method is shown to successfully predict the Nino 3.4 index in a 1998-2017 verification period out to a 10-month lead, which corresponds to an increase of 3-7 months over a benchmark linear inverse model (LIM), while significantly improving upon the ENSO predictability "spring barrier". An analysis of a 1300-yr control integration of a comprehensive climate model (CCSM4) further demonstrates that the enhanced predictability afforded by KAF holds over potentially much longer leads, extending to 24 months versus 18 months in the benchmark LIM.

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