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Retracking of SARAL/AltiKa Radar Altimetry Waveforms for Optimal Gravity Field Recovery

机译:追踪SARAL / AltiKa雷达测高波形以实现最佳重力场恢复

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摘要

The accuracy of the marine gravity field derived from satellite altimetry depends on dense track spacing as well as high range precision. Here, we investigate the range precision that can be achieved using a new shorter wavelength Ka-band altimeter AltiKa aboard the SARAL spacecraft. We agree with a previous study that found that the range precision given in the SARAL/AltiKa Geophysical Data Records is more precise than that of Ku-band altimeter by a factor of two. Moreover, we show that two-pass retracking can further improve the range precision by a factor of 1.7 with respect to the 40 Hz-retracked data (item of range_40 hz) provided in the Geophysical Data Records. The important conclusion is that a dedicated Ka-band altimeter-mapping mission could substantially improve the global accuracy of the marine gravity field with complete coverage and a track spacing of <6 km achievable in similar to 1.3 years. This would reveal thousands of uncharted seamounts on the ocean floor as well as important tectonic features such as microplates and abyssal hill fabric.
机译:从卫星测高仪得出的海洋重力场的精度取决于密集的轨道间距以及高范围的精度。在这里,我们研究了SARAL航天器上使用新型较短波长Ka波段高度计AltiKa可以实现的距离精度。我们同意先前的研究,该研究发现SARAL / AltiKa地球物理数据记录中给出的距离精度比Ku波段高度计的精度高两倍。此外,我们表明,相对于地球物理数据记录中提供的40 Hz跟踪数据(range_40 hz项),两次通过跟踪可以进一步提高测距精度1.7倍。重要的结论是,专门的Ka波段高度计测绘任务可以在1.3年内实现完全覆盖并且轨道间距小于6 km,从而大大提高海洋重力场的全球精度。这将揭示出海床上成千上万的未知海山以及重要的构造特征,例如微板块和深海丘陵构造。

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