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Two-scale model and ocean radar Doppler spectra at moderate- andlow-grazing angles

机译:中度和低度掠角的两尺度模型和海洋雷达多普勒频谱

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摘要

Results of numerical calculations of polarized radar Doppler spectra from the ocean surface at low-grazing angles and at various wind speeds are presented. Calculations are based on the modified two-scale model, which includes Bragg scattering from both free and bound capillary waves. Here, we derive an analytical expression for the Doppler spectrum in the form of a two-dimensional (2-D) integral over large-scale slopes. For the surface description, the model of a directional wave spectrum is used, which takes into account the wave age (a limited fetch). A comparison of computed curves with experimentally measured Doppler spectra shows that the inclusion of “fast” bound capillary waves significantly improves results. Using reasonable parameter values for the model of bound waves we obtained widths of Doppler spectra which are in good agreement with experiments for low-grazing angles θg=10° and for winds up to U 10~10 m/s. However, the remaining discrepancies show that using Bragg scattering from bound waves is not enough to close the problem. Despite limitations the approach can be used for a more thorough analysis of measured Doppler spectra in order to determine the contributions of various scattering mechanisms
机译:给出了在低掠角和不同风速下从海洋表面极化雷达多普勒频谱的数值计算结果。计算基于修改后的两尺度模型,该模型包括来自自由毛细管波和束缚毛细管波的布拉格散射。在这里,我们以大范围斜率上的二维(2-D)积分形式导出了多普勒频谱的解析表达式。对于表面描述,使用了定向波谱模型,该模型考虑了波龄(有限的提取)。计算曲线与实验测量的多普勒光谱的比较表明,包含“快速”束缚毛细管波可显着改善结果。对于束缚波模型,使用合理的参数值,我们获得了多普勒谱的宽度,该宽度与低掠角θg= 10°以及风向U 10〜10 m / s的实验非常吻合。然而,剩余的差异表明,使用束缚波的布拉格散射不足以解决问题。尽管存在局限性,该方法仍可用于对测得的多普勒光谱进行更彻底的分析,从而确定各种散射机制的作用

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