Reconstructing Sea-States in the Southern Ocean Using Ship Motion Data

Filippo Nelli, A. Van Zuydam, K. Pferdekamper, A. Alberello, Marzieh H. Derkani, A. Bekker, A. Toffoli
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引用次数: 1

Abstract

Sea state conditions can be estimated from the motion of a moving ship by converting its response to incident waves through the response amplitude operator. The method is applied herein to ship motion data from the icebreaker R/V Akademik Tryoshnikov and recorded during the Antarctic Circumnavigation Expedition across the Southern Ocean during the Austral summer 2016–17. The response amplitude operator of the vessel was estimated using two boundary element method models, namely NEMOH and HydroSTAR. An inter-comparison of model performance is discussed. The accuracy of the reconstructed sea states is assessed against concurrent measurements of the wave energy spectrum, which were acquired during the expedition with the marine radar WaMoS-II. Results show good agreement between reconstructed sea states (wave spectrum as well as integrated parameters) and direct observations. Model performances are consistent. Nevertheless, NEMOH produces slightly more accurate wave parameters when quantitatively compared against HydroSTAR.
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利用船舶运动数据重建南大洋海况
通过响应幅度算子将运动船舶的响应转换为入射波,可以从运动船舶的运动中估计海况。本文将该方法应用于破冰船R/V Akademik Tryoshnikov的船舶运动数据,这些数据是在2016-17年南极夏季穿越南大洋的南极环游考察期间记录的。采用NEMOH和HydroSTAR两种边界元法模型估计了船舶的响应幅值算子。讨论了模型性能的相互比较。重建海况的准确性是根据在考察期间使用海洋雷达WaMoS-II获得的波浪能谱的同时测量来评估的。结果表明,重建海况(波谱和综合参数)与直接观测结果吻合较好。模型性能是一致的。然而,与HydroSTAR相比,NEMOH在定量上产生的波参数略准确。
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