Abstract

This study validated wind speed (WS) and significant wave height (SWH) retrievals from the Sentinel-3A/3B and Jason-3 altimeters for the period of data beginning 31 October 2019 (to 18 September 2019 for Jason-3) using moored buoy data and satellite Meteorological Operational Satellite Program (MetOp-A/B) Advanced Scatterometer (ASCAT) data. The spatial and temporal scales of the collocated data were 25 km and 30 min, respectively. The statistical metrics of root mean square error (RMSE), bias, correlation coefficient (R), and scatter index (SI) were used to validate the WS and SWH accuracy. Validation of WS against moored buoy data indicated errors of 1.19 m/s, 1.13 m/s and 1.29 m/s for Sentinel-3A, Sentinel-3B and Jason-3, respectively. The accuracy of Sentinel-3A/3B WS is better than that of Jason-3. All three altimeters underestimated WS slightly in comparison with the buoy data. Errors in WS at different speeds or SWHs increased slightly as WS or SWH increased. Over time, the accuracy of the Jason-3 altimeter-derived WS improved, whereas that of Sentinel-3A showed no temporal dependence. The WSs of the three altimeters were compared with ASCAT wind data for validation purposes over the global ocean without in situ measurements. On average, the WSs of the three altimeters were lower in comparison with the ASCAT data. The accuracy of the three altimeters was found to be consistent and stable at low/medium speeds but it decreased when the WS exceeded 15 m/s. Validations of SWH against buoy wave data indicated that the accuracy of Jason-3 SWH was better than that of Sentinel-3A/3B. However, the accuracy of all three altimeters decreased when the SWH exceeded 4 m. The accuracy of Sentinel-3A and Jason-3 SWH was temporally stable, whereas that of Sentinel-3B SWH improved over time. Analyses of SWH accuracy as a function of wave period showed that the Jason-3 altimeter was better than the Sentinel-3A/3B altimeters for long-period ocean waves. Generally, the accuracy of WS and SWH data derived by the Sentinel-3A/3B and Jason-3 altimeters satisfies their mission requirements. Overall, the accuracy of WS (SWH) derived by Sentinel-3A/3B (Jason-3) is better than that retrieved by Jason-3 (Sentinel-3A/3B).

Highlights

  • Sea surface wind is an important parameter of the marine dynamic environment

  • This study evaluated the accuracy of the wind speed (WS) and significant wave height (SWH) retrievals from the Sentinel-3A (1 March 2016 to 31 October 2019), Sentinel-3B (10 November 2018 to 31 October 2019), and Jason-3 (12 February 2016 to 18 September 2019) altimeters using measurements from moored buoys and the MetOp-A/B Advanced Scatterometer (ASCAT)

  • The accuracy of the WS derived by the Sentinel-3A/3B and Jason-3 altimeters over the global ocean and at different WSs and SWHs was analyzed, and the WSs retrieved by the three altimeters were compared with ASCAT data over the global ocean without in situ measurement

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Summary

Introduction

Sea surface wind is an important parameter of the marine dynamic environment. It is related to all types of movement of sea water, e.g., capillary gravity waves, ocean waves, and ocean currents. The accuracy of the WS derived by the Sentinel-3A/3B and Jason-3 altimeters over the global ocean and at different WSs and SWHs was analyzed, and the WSs retrieved by the three altimeters were compared with ASCAT data over the global ocean without in situ measurement. The accuracy of SWHs derived by the Sentinel-3A/3B and Jason-3 altimeters over the global ocean was analyzed at different SWHs, WSs and wave periods.

Results
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