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THE SAR MEASUREMENT OF OCEAN WAVES:WAVE SESSION WHITEPAPER

机译:海洋波浪的SAR测量:波场白皮书

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Remote sensing techniques enable the measurement ofrnocean wave fields with both high resolution and largerncoverage. As the acquisition of active radar data isrnindependent of daylight and cloud conditions, theserndata are therefore believed to be most suited forrnoperational use at weather centers and governmentalrnagencies, as well as for many ongoing scientificrninvestigations. In the present overview paper therndetermination of sea state parameters from radarrnimages together with some results from the operationalrnuse at weather centers are given.rnSynthetic aperture radar (SAR) yields high resolutionrntwo dimensional images of the radar backscatterrnproperties of the sea surface and can thus be used tornmeasure wind fields and sea state from space.rnThe determination of ocean wave spectra from SARrnimage spectra is sensitive to various imaging effectsrndue to sea surface features, spatial variation of windrnspeed, rain, current and motion of the sea surface.rnThus, measuring ocean wave parameters is related tornmost of the other measurements of marine parametersrndescribed in this volume.rnIn this paper an overview of the SAR satelliternmissions is given, as well as a description of the basicrntechniques to measure ocean waves by SAR andrnvalidation against wave model results and other spacernborne and in situ measurements.rnThe full two dimensional SAR image spectrumrnprovides information on the directional ocean wavernspectrum. This can be used to determine expectationrnvalues of, e.g. , significant wave height, mean wavelength and direction in order to improve the wavernmodel prediction. In addition information can berngathered from the radar images directly such asrnindividual wave height, crest length and groupiness ofrnthe ocean waves. Thus, the distribution of maximumrnwave height can be investigated globally, or wavernrefraction and diffraction in coastal areas can bernstudied in detail.rnIn the following an overview of ocean wavernmeasurements from space are given, the papersrnpresented in the wave session are put into the generalrncontext and applications for weather prediction, shiprnrouting, oil and shipbuilding industry and shiprnclassifying societies are discussed.rnA general overview on theory and measurement ofrndirectional wave spectra, including a special chapter onrnremote sensing of directional ocean wave spectrarntogether with an extensive literature list is given in thernCOST Book (2004).
机译:遥感技术可以测量高分辨率和大覆盖率的海平面波场。由于主动雷达数据的获取不依赖于日光和云的条件,因此,serndata被认为最适合在气象中心和政府机构以及许多正在进行的科学调查中进行作战使用。在本概述文件中,给出了雷达图像海状态参数的确定以及气象中心的操作用途的一些结果。合成孔径雷达(SAR)产生了高分辨率的雷达图像,即海面雷达背向散射特性的二维图像,因此可以用于测量从SAR图像光谱中确定海浪光谱对各种成像效果很敏感-由于海面特征,风速,雨水,海流和海面运动的空间变化。-因此,测量海浪参数为与本卷中描述的大多数其他海洋参数测量有关完整的二维SAR图像年龄谱提供有关定向海浪谱的信息。这可以用于确定例如的期望值。 ,重要的波高,平均波长和方向,以改善波模型的预测。另外,可以直接从雷达图像中获取信息,例如单个波高,波峰长度和海浪的聚集度。因此,可以整体研究最大波高的分布,或者可以详细研究沿海地区的波折射和绕射。在下面对从空间进行海浪测量的概述中,将在海浪会议上介绍的论文放到一般的语境和应用中。在气象预报,船舶制造,石油和造船业以及船舶分类学会等方面进行了讨论。方向性波谱的理论和测量概述,包括关于方向性海浪波谱的遥感的特殊章节,以及在成本手册(2004)中给出的详尽文献清单)。

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