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Sea Ice Detection in the Sea of Okhotsk Using PALSAR and MODIS Data

机译:利用PALSAR和MODIS数据检测鄂霍次克海中的海冰

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摘要

In this paper, we propose a new method for improving detection of sea ice through use of PALSAR (Phased-Array type L-band SAR) polarimetric data. Unlike traditional methods that are based on backscattering coefficient, our proposed method utilizes scattering entropy to detect sea ice. We tested this method by comparing sea ice area derived from PALSAR fully polarimetric data covering the Sea of Okhotsk acquired in 2009 and 2010 to that derived from reference MODIS (Moderate Resolution Imaging Spectroradiometer) data of the same region. We applied discriminant analysis to samples of sea ice and open water to determine the threshold of PALSAR backscattering coefficient and scattering entropy needed to discriminate sea ice from open water. We found that sea ice area derived from PALSAR data was equivalent to that derived from MODIS data, suggesting that our proposed method was reliable in the detection of sea ice in the Sea of Okhotsk.
机译:在本文中,我们提出了一种通过使用PALSAR(相控阵型L波段SAR)极化数据改善海冰检测的新方法。与基于后向散射系数的传统方法不同,我们提出的方法利用散射熵检测海冰。我们通过比较从2009年和2010年获得的覆盖鄂霍次克海的PALSAR全极化数据得出的海冰面积与从同一地区的参考MODIS(中等分辨率成像光谱仪)数据得出的海冰面积进行了比较,从而测试了该方法。我们对海冰和开阔水的样本进行了判别分析,以确定区分海冰与开阔水域所需的PALSAR背散射系数和散射熵的阈值。我们发现,从PALSAR数据得出的海冰面积等于从MODIS数据得出的海冰面积,这表明我们提出的方法对于鄂霍次克海中的海冰检测是可靠的。

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