Daily-scale spatiotemporal prediction of thin sea ice thickness during the early freezing season based on EOF-Trans

The accelerated decline of Arctic sea ice is profoundly reshaping regional climate regimes. Sea ice thickness (SIT), particularly under thin-ice conditions, is an important indicator for assessing early-season Arctic sea ice variability, and accurate prediction of its spatiotemporal evolution during the early freezing period is essential for characterizing short-term sea ice changes. In recent years, deep learning has emerged as a complementary approach to traditional sea ice prediction methods. However, existing deep learning-based studies have not fully exploited the large-scale spatial patterns and temporal contextual dependencies inherent in satellite-derived sea ice thickness. To address this limitation, this study proposes a spatiotemporal prediction framework named EOF-Trans for predicting daily-scale variability of thin sea ice thickness during the early freezing season. The method employs Empirical Orthogonal Functions (EOF) to decompose the sea ice thickness field into temporal mode series, utilizes a Transformer architecture to learn the temporal evolution characteristics, and subsequently reconstructs the predicted outputs back into the spatial thickness field by EOF, thereby enabling spatiotemporal sea ice prediction up to a leadtime of 21 days. Experimental results in the Beaufort Sea indicate that the proposed EOF-Trans framework significantly outperforms numerical models and classical deep learning architectures such as U-Net and ConvLSTM. On the 2022–2023 test set, it achieves a correlation coefficient of 88.04%, representing a 2% improvement over U-Net. Even at a leadtime of 21 days, the correlation remains approximately 84%, with the maximum spatial bias not exceeding 0.5 m. These results indicate that EOF-Trans effectively captures spatiotemporal regularities present in thin sea ice thickness, providing a complementary data-driven perspective for short-term sea ice prediction during the early freezing season.

Authors

Institutions

Publication Details

Journal
Frontiers in Marine Science
Published
2026-02-16
DOI
https://doi.org/10.3389/fmars.2026.1657592
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
Field-Weighted Citation Impact
0.00

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Daily-scale spatiotemporal prediction of thin sea ice thickness during the early freezing season based on EOF-Trans

Dandi Wang, Jikun Liu, Pengcheng Li, Ming Gao et al.
Frontiers in Marine Science
Arctic and Antarctic ice dynamics
article

Daily-scale spatiotemporal prediction of thin sea ice thickness during the early freezing season based on EOF-Trans

Dandi Wang, Jikun Liu, Pengcheng Li, Ming Gao, Bo Zheng, Shuai Xing, Guoping Zhang
article en

Abstract

The accelerated decline of Arctic sea ice is profoundly reshaping regional climate regimes. Sea ice thickness (SIT), particularly under thin-ice conditions, is an important indicator for assessing early-season Arctic sea ice variability, and accurate prediction of its spatiotemporal evolution during the early freezing period is essential for characterizing short-term sea ice changes. In recent years, deep learning has emerged as a complementary approach to traditional sea ice prediction methods. However, existing deep learning-based studies have not fully exploited the large-scale spatial patterns and temporal contextual dependencies inherent in satellite-derived sea ice thickness. To address this limitation, this study proposes a spatiotemporal prediction framework named EOF-Trans for predicting daily-scale variability of thin sea ice thickness during the early freezing season. The method employs Empirical Orthogonal Functions (EOF) to decompose the sea ice thickness field into temporal mode series, utilizes a Transformer architecture to learn the temporal evolution characteristics, and subsequently reconstructs the predicted outputs back into the spatial thickness field by EOF, thereby enabling spatiotemporal sea ice prediction up to a leadtime of 21 days. Experimental results in the Beaufort Sea indicate that the proposed EOF-Trans framework significantly outperforms numerical models and classical deep learning architectures such as U-Net and ConvLSTM. On the 2022–2023 test set, it achieves a correlation coefficient of 88.04%, representing a 2% improvement over U-Net. Even at a leadtime of 21 days, the correlation remains approximately 84%, with the maximum spatial bias not exceeding 0.5 m. These results indicate that EOF-Trans effectively captures spatiotemporal regularities present in thin sea ice thickness, providing a complementary data-driven perspective for short-term sea ice prediction during the early freezing season.

Frontiers in Marine ScienceVol. 13
Smart Material (Germany) (DE)
National Natural Science Foundation of China, Natural Science Foundation of Henan Province
Life below water
Openalex Percentile: Top 66%
Arctic and Antarctic ice dynamics
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.