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首页> 外文期刊>IEEE Transactions on Geoscience and Remote Sensing >Arctic Sea Ice Classification Using Microwave Scatterometer and Radiometer Data During 2002–2017
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Arctic Sea Ice Classification Using Microwave Scatterometer and Radiometer Data During 2002–2017

机译:2002-2017年期间使用微波散射仪和辐射计数据对北极海冰进行分类

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摘要

Temporal and spatial variation of sea ice type in the Arctic is an indicator of regional and global change. Arctic sea ice can be classified into two major categories: multiyear ice (MYI) and first-year ice. In this paper, classification method based on machine learning is established and applied to produce daily sea ice classification data set during the winter (November-April) from 2002 to 2017 using active microwave data from QuikSCAT and Advanced Scatterometer as well as passive microwave data from Advanced Microwave Scanning Radiometer for EOS, Special Sensor Microwave Imager/Sounder, and Advanced Microwave Scanning Radiometer 2 radiometer. First, the open water area is flagged out using brightness temperature (Tb) from the passive microwave sensor. Then, K-means algorithm is applied to identify the clusters of the two ice types in the Tb/backscatter parameter space and finally assign pixels to each class. Two optimization methods based on the movement of MYI and marginal ice zone are used to correct the misclassification of MYI. The results have shown a decrease of MYI in winter from 2002 to 2017, especially in 2008 and 2013 with a remarkable recovery in 2014. The classifications are consistent with results by visual interpretation from synthetic aperture radar images in the Canadian Arctic Archipelago with overall classification accuracy over 93%. Comparison with classifications from previous studies and products shows that our method could reflect more differences in MYI declining trend interannually and less anomalous fluctuations in certain years.
机译:北极海冰类型的时空变化是区域和全球变化的指标。北极海冰可分为两大类:多年期冰(MYI)和一年级冰。本文建立了基于机器学习的分类方法,并利用QuikSCAT和Advanced Scatterometer的主动微波数据以及被动的微波数据生成了2002年至2017年冬季(11月至4月)的每日海冰分类数据集。用于EOS的高级微波扫描辐射仪,特殊传感器微波成像仪/测深仪和高级微波扫描辐射仪2辐射仪。首先,使用来自无源微波传感器的亮度温度(Tb)标记出开放水域。然后,使用K-means算法在Tb /反向散射参数空间中识别两种冰类型的聚类,最后将像素分配给每个类别。两种基于MYI运动和边缘冰区的优化方法用于纠正MYI的错误分类。结果表明,2002年至2017年冬季,尤其是2008年和2013年,冬季的MYI有所下降,2014年出现了显着恢复。分类与加拿大北极群岛合成孔径雷达图像的视觉解释结果一致,总体分类准确超过93%。与以往研究和产品分类的比较表明,我们的方法可以反映出MYI逐年下降趋势的差异更大,并且在某些年份中反常波动较小。

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