用自适应时空聚类提升海洋温盐数据重建精度
An Adaptive Spatiotemporal Clustering Framework for 3D Ocean Subsurface Temperature Reconstruction

- 通过时空聚类捕捉海水温度垂直结构与时间变化规律
- 相比原始模型,误差降低12.4%至27.2%
- 适合气候建模与海洋动力研究者使用
利用卫星遥感数据重建海洋次表层温度(OST)对理解海洋动力学和气候变异具有重要意义。然而,次表层观测稀缺,且过程高度非线性、时空异质性强,制约了传统重建方法的准确性和泛化能力。本文提出一种自适应框架,通过时空聚类捕获OST的垂直结构依赖关系与时间演变模式。该框架可与多种深度学习模型(如双路径卷积神经网络DP-CNN、Attention U-Net、Vision Transformer)结合,仅基于表层观测(海表温度SST、海表盐度SSS、海表高SSH、海表风SSW)实现全球尺度的OST精确重建。实验表明,引入该框架后,多个模型在均方根误差(RMSE)上相较原模型提升12.4%至27.2%。本研究为次表层温度重建提供了可靠方案,对气象建模与气候变化评估具有重要价值。
原文摘要 · Abstract (English)
The reconstruction of ocean subsurface temperature (OST) using satellite remote sensing data holds significant scientific value for advancing the understanding of ocean dynamics and climate variability. However, the scarcity of subsurface observations, combined with the high degree of nonlinearity and spatiotemporal heterogeneity in subsurface processes, poses substantial challenges to the accuracy and generalization capability of traditional reconstruction methods. To address these limitations, this study proposes an adaptive framework that could capture both vertical structural dependencies and temporal variation patterns of OST via spatio-temporal clustering. By incorporating this framework with various deep learning models, e.g., dual-path convolutional neural networks (DP-CNN), Attention U-Net, and Vision Transformer (ViT), the OST field can be accurately reconstructed at a global scale only using surface observations, i.e., sea surface temperature (SST), sea surface salinity (SSS), sea surface height (SSH), and sea surface wind (SSW). Experimental results demonstrate that multiple deep learning methods using the proposed framework largely outperform their original counterparts, yielding improvements in RMSE ranging from 12.4\% to 27.2\%. This study provides a reliable solution for subsurface temperature reconstruction, offering important implications for meteorological modeling and climate change assessment.
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