AO-PHAILGDec 15, 2023

FuXi-S2S: A machine learning model that outperforms conventional global subseasonal forecast models

arXiv:2312.09926v25 citationsh-index: 18
Originality Highly original
AI Analysis

This provides improved subseasonal forecasts for sectors like agriculture and disaster management, representing a novel method for a known bottleneck.

The paper tackles the challenge of subseasonal weather forecasting by introducing FuXi-S2S, a machine learning model that outperforms the ECMWF's state-of-the-art model in ensemble forecasts for precipitation and outgoing longwave radiation, extending skillful MJO prediction from 30 to 36 days.

Skillful subseasonal forecasts are crucial for various sectors of society but pose a grand scientific challenge. Recently, machine learning based weather forecasting models outperform the most successful numerical weather predictions generated by the European Centre for Medium-Range Weather Forecasts (ECMWF), but have not yet surpassed conventional models at subseasonal timescales. This paper introduces FuXi Subseasonal-to-Seasonal (FuXi-S2S), a machine learning model that provides global daily mean forecasts up to 42 days, encompassing five upper-air atmospheric variables at 13 pressure levels and 11 surface variables. FuXi-S2S, trained on 72 years of daily statistics from ECMWF ERA5 reanalysis data, outperforms the ECMWF's state-of-the-art Subseasonal-to-Seasonal model in ensemble mean and ensemble forecasts for total precipitation and outgoing longwave radiation, notably enhancing global precipitation forecast. The improved performance of FuXi-S2S can be primarily attributed to its superior capability to capture forecast uncertainty and accurately predict the Madden-Julian Oscillation (MJO), extending the skillful MJO prediction from 30 days to 36 days. Moreover, FuXi-S2S not only captures realistic teleconnections associated with the MJO, but also emerges as a valuable tool for discovering precursor signals, offering researchers insights and potentially establishing a new paradigm in Earth system science research.

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