Paper
27 November 2024 Spatio-temporal prediction model for sea ice density based on ConvLSTM network
Xiangyu Zhao, Zhiyong Wang, Shunwei Liu
Author Affiliations +
Proceedings Volume 13402, International Conference on Remote Sensing, Mapping, and Geographic Information Systems (RSMG 2024); 134023D (2024) https://doi.org/10.1117/12.3048720
Event: International Conference on Remote Sensing, Mapping, and Geographic Information Systems (RSMG 2024), 2024, Zhengzhou, China
Abstract
Aiming at the problem that the traditional deep learning prediction model has low accuracy in predicting sea ice density and is difficult to capture the spatiotemporal variation of sea ice density, this paper constructed an improved spatiotemporal prediction model ConvLSTM to predict the Arctic sea ice density. A deep learning network was used to capture temporal and spatial changes in Arctic sea ice density over a 45-year period. Finally, the monthly average data of 2023 is output and displayed as the result. The results show that compared with the traditional prediction model, the proposed model is superior to the LSTM algorithm in prediction accuracy. LSTM network can overestimate the extent of sea ice density data to different degrees, especially in the melting season of sea ice, and ConvLSTM model has a better performance. The RMSE, MSE, MAE, R2 and SSIM of the model in this paper are 0.0644, 0.0043, 0.0145, 0.9318 and 0.9427, respectively.
(2024) Published by SPIE. Downloading of the abstract is permitted for personal use only.
Xiangyu Zhao, Zhiyong Wang, and Shunwei Liu "Spatio-temporal prediction model for sea ice density based on ConvLSTM network", Proc. SPIE 13402, International Conference on Remote Sensing, Mapping, and Geographic Information Systems (RSMG 2024), 134023D (27 November 2024); https://doi.org/10.1117/12.3048720
Advertisement
Advertisement
RIGHTS & PERMISSIONS
Get copyright permission  Get copyright permission on Copyright Marketplace
KEYWORDS
Ice

Data modeling

Deep learning

Education and training

Convolution

Climate change

Climatology

Back to Top