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首页> 外文期刊>IEEE Transactions on Geoscience and Remote Sensing >Thin saline ice thickness retrieval using time-series C-band polarimetric radar measurements
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Thin saline ice thickness retrieval using time-series C-band polarimetric radar measurements

机译:使用时间序列C波段极化雷达测量结果获取稀薄的冰层厚度

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The application of time-series radar measurements to accurately invert the thickness of saline ice is presented in this study. The authors describe briefly some experimental observations from the United States Army Cold Regions Research and Engineering Laboratory, Hanover, NH, 1993 (CRRELEX'93) campaign of microwave scattering from sea ice. They demonstrate that volume scattering from brine inclusions is an important contribution to the backscatter response of saline ice in this case. From the experimental findings and the thermophysics of ice growth, they develop an inversion algorithm for the ice thickness based on a dynamic electromagnetic scattering model of saline ice. This inversion algorithm uses a parametric estimation approach in which the radiative transfer equation is used as the direct scattering model to calculate the backscattering signatures from ice medium and the Levenberg-Marquardt method is employed to retrieve ice thickness iteratively. Additional information provided by the saline ice thermodynamics is applied to constrain the electromagnetic inverse problem to achieve a reasonably accurate reconstruction. The inversion results using this algorithm and the data from CRRELEX'93 experiment are compared. The accurate thickness retrieval suggests the potential use of this algorithm for retrieving geophysical parameters from satellite remote-sensing data.
机译:在这项研究中,应用了时间序列雷达测量来准确地反转盐冰的厚度。作者简要介绍了来自美国陆军寒区研究与工程实验室(1993年,新罕布什尔州汉诺威)(CRRELEX'93)从海冰中进行微波散射的一些实验观察结果。他们证明,在这种情况下,盐水夹杂物的体积散射是对盐冰的反向散射响应的重要贡献。根据实验结果和冰块生长的热物理学,他们基于盐冰的动态电磁散射模型开发了一种反演冰厚度的算法。该反演算法使用参数估计方法,其中将辐射传递方程用作直接散射模型,以计算冰介质的反向散射特征,并采用Levenberg-Marquardt方法迭代地获取冰厚。盐冰热力学提供的其他信息可用于约束电磁逆问题,以实现合理准确的重构。比较了使用该算法的反演结果和来自CRRELEX'93实验的数据。准确的厚度检索表明该算法可能用于从卫星遥感数据中检索地球物理参数。

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