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Dominant Wave Directions and Significant Wave Heights from Synthetic Aperture Radar Imagery of the Ocean

机译:海洋合成孔径雷达图像的主导波方向和重要波高

摘要

We show that quasi-linear theory accounts for dominant wave directions observed in synthetic aperture radar (SAR) imagery of the ocean for range-to-velocity (R/V) ratios up to 70 s. We also show that when used in combination with Alpers and Hasselmannu27s [1982] model of signal-to-noise ratios in SAR imagery, this theory yields significant wave heights in good agreement with those actually observed. We have found that the apparent dominant wave direction in SAR imagery taken at a 45° incidence angle can differ from the true wave direction by as much as 40° under certain conditions. To understand such differences, we simulated SAR image spectra using quasi-linear theory, a surface wave spectrum measured by a buoy but with a variable angular spread, coherence times calculated from line-of-sight velocity spreads, and modulation transfer functions based on a functional form developed from Bragg scattering theory and data obtained during the SAR X Band Ocean Nonlinearities-Forschungsplatform Nordsee (SAXON-FPN) experiment. We carried out these simulations for a 45° incidence angle, L, C, and X bands, both horizontal/horizontal (HH) and vertical/vertical (VV) polarization, three different flight altitudes, and a variety of flight directions to compare the predicted apparent wave directions with those observed in the SAR imagery collected during SAXON-FPN. The difference between the SAR-derived dominant wave direction and the one measured by the buoy could be predicted well as a function of the true wave direction relative to the flight direction. The parameters of the quasi-linear theory that produced the best fit to the directional data differed somewhat from those measured by tower-based radars during SAXON-FPN, however. Significant wave heights obtained using the parameters that best fit the directional data were in good agreement with those measured by the buoy. The SAR-derived wave heights were consistently higher than the measured ones, however, unless the full system bandwidth was used in determining the clutter level, that is, unless bandwidth reductions due to azimuthal presumming and multilook averaging were removed. Finally, the prediction and observation of spectral splitting in SAR spectra of azimuthally traveling waves are also reported.
机译:我们显示准线性理论解释了在长达70 s的距离-速度(R / V)比的海洋的合成孔径雷达(SAR)图像中观察到的主导波方向。我们还表明,与SAR图像中信噪比的Alpers和Hasselmann u27s [1982]模型结合使用时,该理论产生的波高与实际观测的波高高度吻合。我们已经发现,在某些条件下,以45°入射角拍摄的SAR图像中的表观优势波方向可能与真实波方向相差40°。为了理解这种差异,我们使用准线性理论模拟SAR图像光谱,通过浮标测量但具有可变角展度的表面波光谱,根据视线速度展度计算的相干时间,以及基于a的调制传递函数。功能形式是根据布拉格散射理论发展而来,并在SAR X波段海洋非线性— Forschungs平台Nordsee(SAXON-FPN)实验中获得了数据。我们针对45°入射角,L,C和X波段,水平/水平(HH)和垂直/垂直(VV)极化,三种不同的飞行高度以及各种飞行方向进行了这些仿真,以比较与在SAXON-FPN期间收集的SAR图像中观察到的那些相一致的预测波方向。 SAR衍生的主波方向与浮标测量的方向之间的差异可以很好地预测为相对于飞行方向的真实波方向的函数。但是,准线性理论的参数与方向性数据最匹配,但与SAXON-FPN期间塔式雷达测量的参数有些不同。使用最适合方向数据的参数获得的重要波高与浮标所测得的波高高度吻合。 SAR衍生的波高始终高于被测SAR的波高,但是,除非使用整个系统带宽来确定杂波电平,也就是说,除非消除了由于方位角推测和多视点平均引起的带宽降低。最后,还报道了方位角行波SAR谱中谱分裂的预测和观察。

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