首页> 外文会议>Geoscience and Remote Sensing Symposium, 2004. IGARSS '04. Proceedings. 2004 IEEE International >Study on the sea ice thickness observation in the Sea of Okhotsk by using dual-frequency and fully polarimetric airborne SAR (Pi-SAR) data
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Study on the sea ice thickness observation in the Sea of Okhotsk by using dual-frequency and fully polarimetric airborne SAR (Pi-SAR) data

机译:利用双频和全极化机载SAR(Pi-SAR)数据研究鄂霍次克海的海冰厚度

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The Sea of Okhotsk is located in the most southerly region of the Northern Hemisphere in which sea ice exists during winter. Since the area and volume of the sea ice in this region are related to climate change locally as well as globally, it is important to develop methods for monitoring sea ice parameters around this region. Since Synthetic Aperture Radar (SAR) can observe continuously in any weather conditions, it is useful for observing the sea ice covered region. In order to investigate the possibilities of dual frequency and polarimetric SAR to monitor the sea ice, we derived the relation between backscattering coefficients each polarization and sea ice physical parameters, and then we proposed a sea ice classification using a polarimetric decomposition and a sea ice thickness estimation using the backscatter ratio.
机译:鄂霍次克海位于北半球最南端的区域,冬季存在海冰。由于该地区海冰的面积和数量与本地乃至全球气候变化有关,因此开发监测该地区海冰参数的方法很重要。由于合成孔径雷达(SAR)可以在任何天气条件下连续观察,因此对于观察海冰覆盖区域非常有用。为了研究双频和极化SAR监测海冰的可能性,我们推导了每个极化的反向散射系数与海冰物理参数之间的关系,然后提出了利用极化分解和海冰厚度的海冰分类方法。使用后向散射比进行估算。

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