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Tidal deflection of Ross Ice Shelf, Antarctica, observed by Sentinel-1A double-differential interferometric SAR

机译:Sentinel-1A双差分干涉SAR观测到的南极罗斯冰架的潮汐挠度

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This paper reports the tidal deflection of Ross Ice Shelf, Antarctica, observed from Sentinel-1A data processed by using double-differential interferometric synthetic aperture radar (DDInSAR) technique. Sentinel-1A single look complex SAR data of 2015-2016, along the east and the west coast of Ross Ice Shelf, were obtained and interferometrically processed by Sentinel Application Platform (SNAP) program. GETASSE30 digital elevation model was used to remove the topographic fringes. After the phase unwrapping using SNAPHU program, the two interferograms were subtracted to obtain DDInSAR image to highlight the tidal deflection signals under the assumption of steady gravitational glacial flow. As a result, we can identify grounding lines and hinge zones in the east and the west coast of Ross Ice Shelf. The wider hinge zone in the west indicates thicker ice shelf than the east. Comparison of the tidal deflection with tidal model remind us the importance of barometric correction.
机译:本文报告了南极罗斯冰架的潮汐挠度,该潮汐挠度是通过使用双差分干涉合成孔径雷达(DDInSAR)技术处理的Sentinel-1A数据观察到的。通过Sentinel应用程序平台(SNAP)程序获取了沿Ross冰架东,西海岸的2015-2016年Sentinel-1A单看复杂SAR数据,并对其进行了干涉测量。 GETASSE30数字高程模型用于去除地形条纹。在使用SNAPHU程序进行相位展开之后,将两个干涉图相减以获得DDInSAR图像,以突出显示在稳定重力冰流作用下的潮汐偏转信号。结果,我们可以确定罗斯冰架东海岸和西海岸的接地线和铰链区。西部较宽的铰链区表示冰架比东部更厚。潮汐挠度与潮汐模型的比较提醒我们气压校正的重要性。

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