首页> 外文会议>2011 4th International Congress on Image and Signal Processing >A coastal acoustic tomography inverse method based on Legendre polynomials and its application in Sanmen Bay field experiment, China
【24h】

A coastal acoustic tomography inverse method based on Legendre polynomials and its application in Sanmen Bay field experiment, China

机译:基于勒让德多项式的海岸声层析成像反演方法及其在中国三门湾野外实验中的应用

获取原文

摘要

Seven sets of shelf-contained type coastal acoustic tomography systems (CATs) were successfully deployed in Sammen Bay near the Taizhou city, China, during September 6 to 9, 2009 to measure tidal current structures at 3-min interval. An inverse model based on Legendre polynomials and Tikhonov regularization technology is developed to reconstruct the tidal current distributions using travel time differences obtained from the reciprocal sound transmission between the paired CAT stations. Variation of tidal current fields from food tide to ebb tide and tidal vortexes are well reconstructed. The horizontal distributions of tidal current obtained from the inverse analysis are in good agreement with that of Acoustic Doppler current Profiler (ADCP) observation and FVCOM ocean model. Comparison between CAT inversion and FVCOM model results, the spatial averaged mean square deviation (RMSD) is about 0.09 m/s for the eastward current and 0.04 m/s for the northward current, respectively. The time average RMSD between CAT inversion and ADCP measurement is 0.09 m/s for eastward current component and 0.002 m/s for northward current component, respectively. The investigation suggests that the coastal acoustic tomography inverse method based on Legendre polynomials is a promising alternative method for the ocean acoustic tomography inverse problem.
机译:2009年9月6日至9日,在中国台州市附近的三门湾成功部署了7套搁板式海岸声波层析成像系统(CAT),以3分钟的间隔测量潮流结构。建立了基于勒让德多项式和Tikhonov正则化技术的逆模型,以利用从成对CAT站之间的相互声音传输获得的传播时间差来重建潮流分布。潮汐场从食物潮汐到退潮和潮汐涡的变化都得到了很好的重建。反演得到的潮流的水平分布与声多普勒潮流剖面仪(ADCP)观测和FVCOM海洋模型相吻合。比较CAT反演和FVCOM模型结果,东向洋流的空间平均均方差(RMSD)约为0.09 m / s,北向洋流的空间平均均方差(RMSD)约为0.04 m / s。 CAT反演与ADCP测量之间的平均时间RMSD对于东向电流分量是0.09 m / s,对于北向电流分量是0.002 m / s。研究表明,基于勒让德多项式的海岸声学层析成像反演方法是解决海洋声学层析成像反演问题的一种有前途的替代方法。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号