用深度学习光学流精准估算北极海冰漂移,精度达300米以内。
Towards Reliable Sea Ice Drift Estimation in the Arctic Deep Learning Optical Flow on RADARSAT-2
- 首次在雷达卫星影像上大规模测试48种深度学习光学流模型
- 误差仅6至8像素(300至400米),接近导航要求精度
- 可生成连续漂移场,适合海冰导航与气候建模
准确估计海冰漂移对北极航行、气候研究和业务预报至关重要。尽管光学流作为计算机视觉中估算连续图像间像素级运动的技术发展迅速,其在地球物理问题及卫星合成孔径雷达(SAR)影像中的应用仍较少被探索。传统光学流方法依赖数学模型和强运动假设,在复杂场景下精度受限。近年来基于深度学习的方法显著提升性能,已成为计算机视觉标准,推动其在海冰漂移估计中的应用。本文首次在RADARSAT-2 ScanSAR海冰影像上构建大规模基准,评估48种深度学习光学流模型,以地面真实浮标数据为参考,使用终点误差(EPE)和Fl all指标进行验证。多个模型达到亚千米级精度(EPE 6–8像素,对应300–400米),远小于海冰运动尺度,满足典型北极航行需求。结果表明,这些模型能有效捕捉区域一致的漂移模式,且相比传统方法,深度学习光学流在运动估计精度上实现显著提升,可成功迁移至极地遥感领域。光学流生成空间连续的漂移场,为每个像素提供运动估计,而非仅限于稀疏浮标位置,为航行与气候模拟开辟新可能。
原文摘要 · Abstract (English)
Accurate estimation of sea ice drift is critical for Arctic navigation, climate research, and operational forecasting. While optical flow, a computer vision technique for estimating pixel wise motion between consecutive images, has advanced rapidly in computer vision, its applicability to geophysical problems and to satellite SAR imagery remains underexplored. Classical optical flow methods rely on mathematical models and strong assumptions about motion, which limit their accuracy in complex scenarios. Recent deep learning based approaches have substantially improved performance and are now the standard in computer vision, motivating their application to sea ice drift estimation. We present the first large scale benchmark of 48 deep learning optical flow models on RADARSAT 2 ScanSAR sea ice imagery, evaluated with endpoint error (EPE) and Fl all metrics against GNSS tracked buoys. Several models achieve sub kilometer accuracy (EPE 6 to 8 pixels, 300 to 400 m), a small error relative to the spatial scales of sea ice motion and typical navigation requirements in the Arctic. Our results demonstrate that the models are capable of capturing consistent regional drift patterns and that recent deep learning based optical flow methods, which have substantially improved motion estimation accuracy compared to classical methods, can be effectively transferred to polar remote sensing. Optical flow produces spatially continuous drift fields, providing motion estimates for every image pixel rather than at sparse buoy locations, offering new opportunities for navigation and climate modeling.
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