首页> 外文会议>IEEE International Geoscience and Remote Sensing Symposium >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:用双频和全极化空气传播SAR(PI-SAR)数据研究Okhotsk海洋海冰厚度观察研究

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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:Okhotsk的海景位于北半球最南半球的南半球地区,冬季冰也存在海冰。 由于该地区的海冰的面积和体积与本地以及全球范围内的气候变化有关,因此开发用于监测该地区的海冰参数的方法。 由于合成孔径雷达(SAR)可以在任何天气条件下连续观察,因此它对于观察海冰区域是有用的。 为了调查双频和偏振SAR监测海冰的可能性,我们派生了反向散射系数之间的关系,每个极化和海冰物理参数,然后我们用偏振分解和海冰厚度提出了海冰分类 使用反向散射率估计。

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