首页> 外文会议>International astronautical congress >AN OCEAN WAVE SIMULATOR AS A BASIS FOR MODELLING SAR BACKSCATTERING OF OCEAN WAVE SPECTRA
【24h】

AN OCEAN WAVE SIMULATOR AS A BASIS FOR MODELLING SAR BACKSCATTERING OF OCEAN WAVE SPECTRA

机译:以海浪模拟器为基础的海浪频谱SAR反散射建模

获取原文

摘要

The observation of the ocean surface via spaceborne SAR systems is a difficult task, even at the early stages of both the development and testing of such systems. Indeed, the nature of the ocean dynamics -which can be considered as a chaotic and non-stationary process -prevents from studying fully-deterministic scenarios at a certain degree of accuracy. Due to it is simply impossible to get identical realisations of the ocean surface in the same geographical region but recorded at different times, a numerical ocean wave simulator is proposed here as an alternative way of working with specific scenarios. We say the simulator is able to synthetically generate a fully-deterministic realisation of an artificial ocean surface -at a particular time and space;- when the underlying model is completely known. Furthermore, the idea of producing fully-deterministic realisations docs not imply that the model is rigid. In a statistical sense, the model can be "harmlessly flexible", because the randomness is assumed to be entirely characterised and controlled by the use of certain probability distributions that can keep close relations to theoretical results and empirical observations of the linear wave theory and the ocean wave spectra, respectively. The numerical simulator is intended to produce realisations of the ocean surface that arc close to reality, based on several well-known omnidirectional spectra and spreading functions that arc proposed in the literature. Since this numerical simulator constitutes the basis for the next step of our research work -a better understanding of ocean features by means of the backscattcrcd RCS of the ocean surface roughness using a SAR system- a special emphasis is put on the appropriate construction of the ocean waves that arc visible by the radar, that is, ocean wavelengths in the same magnitude order as the radar wavelength.
机译:即使在此类系统的开发和测试的早期阶段,通过星载SAR系统观察海面也是一项艰巨的任务。确实,海洋动力学的本质(可以被认为是一个混沌且非平稳的过程)可以防止以一定的准确性研究完全确定的情况。由于根本不可能在同一地理区域获得相同的海面实现,而是在不同的时间进行记录,因此在此提出了一种数字海浪模拟器,作为处理特定场景的另一种方法。我们说模拟器可以在特定的时间和空间上综合生成人工海洋表面的完全确定性实现,而底层模型是完全已知的。此外,产生完全确定性实现的想法并不意味着该模型是严格的。从统计意义上讲,该模型可以是“无害灵活的”,因为假定随机性是通过使用某些概率分布来完全表征和控制的,这些概率分布可以与线性波理论和线性波动理论的理论结果和经验观察保持密切的关系。海浪光谱。数值模拟器旨在基于文献中提出的几种众所周知的全向光谱和扩展函数来产生接近现实的海洋表面的实现。由于此数值模拟器构成了我们下一步研究的基础-通过使用SAR系统通过对海面粗糙度的反演RCS更好地了解海洋特征-特别强调了适当的海洋构造雷达可见的电磁波,即与雷达波长相同数量级的海洋波长。

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