New classes of climate model emulators to improve paleoclimate reconstructions
Abstract. Reconstructing spatial climate variability from proxy records requires forward models “emulators” that capture the dynamical structure of the climate system while remaining computationally efficient. Traditional emulators based on Empirical Orthogonal Functions and Linear Inverse Models (LIMs) face inherent limitations due to linearity and variance-based dimensionality reduction. Here we develop and evaluate a hierarchy of CMIP-class climate model emulators that integrate autoencoder-based dimensionality reduction with nonlinear prediction architectures, including Reservoir Computing (RC) and Recurrent Neural Networks (RNNs). Using a comprehensive experimental protocol applied to the IPSL-CM6A-LR model and 52 CMIP6s models, we show that combining autoencoder and RC (AERCn) provides the most robust performance across time scales and dynamical regimes when data are plentiful. The AERCn configuration captures nonlinear features of ENSO and Atlantic Multidecadal Variability, maintains high spatial reconstruction skill, and generalizes across distinct climate model structures. When training data are scarce, a multimodel pre-trained AERNN provides a data-efficient and competitive alternative. These properties make the proposed architectures particularly well suited for integration into Particle Filters and Ensemble Kalman Filter PDA frameworks. Our results highlight the importance of predictability-oriented dimensionality reduction and nonlinear dynamical memory for emulator design, and they provide a scalable path toward improved reconstructions of climate variability over the Common Era.
This study analyzes the limitations of the LIM-EOF model in traditional paleoclimate reconstruction methods. To address these issues, an improved climate model simulator is proposed, targeting the structural deficiencies of the traditional method with three specific improvements. The study evaluates whether these innovative measures enhance the simulation accuracy of large-scale climate variability, improve predictive capability, and reduce simulation errors in extreme events. The research is detailed, thoroughly elaborating on the dimensionality reduction algorithm and prediction model, describing the architecture and implementation of the simulator, and using extensive datasets and climate models to evaluate its multifaceted performance. Simulations based on the CMIP6 model suite demonstrate that the proposed improvements significantly outperform the traditional LIM-EOF model in terms of prediction accuracy, dynamic performance, avoidance of error accumulation, etc. In addition to a detailed analysis of the advantages of these improvements, the study also discusses certain limitations of the simulator under specific conditions, while proposing directions for further research. The work contributes notably to enhancing the accuracy of paleoclimate reconstruction and holds strong exploratory significance for advancing various research methods in the field.
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