Retrieving Ocean Surface Winds and Waves from Augmented Dual-Polarization Sentinel-1 SAR Data Using Deep Convolutional Residual Networks

Author:

Xue Sihan1,Meng Lingsheng12ORCID,Geng Xupu13ORCID,Sun Haiyang13ORCID,Edwing Deanna2ORCID,Yan Xiao-Hai24ORCID

Affiliation:

1. State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China

2. College of Earth, Ocean and Environment, University of Delaware, Newark, DE 19716, USA

3. Engineering Research Center of Ocean Remote Sensing Big Data, Fujian Province University, Xiamen 361005, China

4. Joint Institute for Coastal Research and Management (Joint-CRM), University of Delaware and Xiamen University, Newark, DE 19716, USA

Abstract

Sea surface winds and waves are very important phenomena that exist in the air–sea boundary layer. With the advent of climate change, cascade effects are bringing more attention to these phenomena as warmer sea surface temperatures bring about stronger winds, thereby altering global wave conditions. Synthetic aperture radar (SAR) is a powerful sensor for high-resolution surface wind and wave observations and has accumulated large quantities of data. Furthermore, deep learning methods have been increasingly utilized in geoscience, especially the inversion of ocean information from SAR imagery. Here, we propose a method to invert various parameters of ocean surface winds and waves using Sentinel-1 SAR IW mode data. To ensure this method is more robust and scalable, we augmented the input data with dual-polarized SAR imagery, an incident angle, and a more constrained homogeneity test. This method adopts a deeper structure in order to retrieve more wind and wave parameters, and the use of residual networks can accelerate training convergence and improve regression accuracy. Using 1600 training samples filtered by a novel homogeneity test and with significant wave heights between 0 and 10 m, results from error parameters including the root mean square error (RMSE), scatter index (SI), and correlation coefficient (COR) show the great performance of this proposed method. The RMSE is 0.45 m, 0.76 s, and 1.90 m/s for the significant wave height, mean wave period, and wind speed, respectively. Furthermore, the temporal variation and spatial distribution of the estimates are consistent with China–France Oceanography Satellite (CFOSAT) observations, buoy measurements, WaveWatch3 regional model data, and ERA5 reanalysis data.

Funder

National Key R & D Program of China

National Natural Science Foundation of China

Industry–University Cooperation and Collaborative Education Projects

NSF

NASA

Fujian Haisi Digital Technology Co., Ltd.

Fujian Tendering Purchasing Group Co., Ltd.

Publisher

MDPI AG

Subject

Atmospheric Science,Environmental Science (miscellaneous)

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