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Bibliographic Details
Main Authors: Alboré, Nicola, Di Antonio, Gabriele, Coccetti, Fabrizio, Gabrielli, Andrea
Format: Preprint
Published: 2025
Subjects:
Online Access:https://arxiv.org/abs/2510.11209
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author Alboré, Nicola
Di Antonio, Gabriele
Coccetti, Fabrizio
Gabrielli, Andrea
author_facet Alboré, Nicola
Di Antonio, Gabriele
Coccetti, Fabrizio
Gabrielli, Andrea
contents We propose a new reservoir computing method for forecasting high-resolution spatiotemporal datasets. By combining multi-resolution inputs from coarser to finer layers, our architecture better captures both local and global dynamics. Applied to Sea Surface Temperature data, it outperforms standard parallel reservoir models in long-term forecasting, demonstrating the effectiveness of cross-layers coupling in improving predictive accuracy. Finally, we show that the optimal network dynamics in each layer become increasingly linear, revealing the slow modes propagated to subsequent layers.
format Preprint
id arxiv_https___arxiv_org_abs_2510_11209
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle Cross-Scale Reservoir Computing for large spatio-temporal forecasting and modeling
Alboré, Nicola
Di Antonio, Gabriele
Coccetti, Fabrizio
Gabrielli, Andrea
Machine Learning
Computational Physics
We propose a new reservoir computing method for forecasting high-resolution spatiotemporal datasets. By combining multi-resolution inputs from coarser to finer layers, our architecture better captures both local and global dynamics. Applied to Sea Surface Temperature data, it outperforms standard parallel reservoir models in long-term forecasting, demonstrating the effectiveness of cross-layers coupling in improving predictive accuracy. Finally, we show that the optimal network dynamics in each layer become increasingly linear, revealing the slow modes propagated to subsequent layers.
title Cross-Scale Reservoir Computing for large spatio-temporal forecasting and modeling
topic Machine Learning
Computational Physics
url https://arxiv.org/abs/2510.11209