Abstract

Sea ice classification using synthetic aperture radar (SAR) in the wide-swath mode is one method for ice type retrieval. The conventional method of sea ice classification involves single-scale classification, wherein the backscatter and gray-level co-occurrence matrix features in a specific resolution are used as classification bases. The classification is implemented only once. In this way, however, the scalloping and interscan banding (ISB) artifacts in some TerraSAR-X ScanSAR data affect the classification result. In this article, a two-scale method of sea ice classification is proposed. The two-scale process includes both the coarse- and fine-resolution classifications. First, the coarse-resolution classification utilizes downscale images to generate the ice zone. Subsequently, the fine-scale classification utilizes the full-resolution SAR image and the ice zone to generate the final classification result. The support vector machine is used as the classifier. This two-scale method provides a better classification result compared to the single-scale method in two aspects. First, it effectively avoids the appearance of scalloping and ISB artifacts in the results. Second, it is less time-consuming and provides satisfactory results for discriminating multiyear ice, first-year ice, and water. The validation is accomplished using independent images, with an overall average accuracy of 86.38%. This article shows that this method may provide an alternative for sea ice classification using TerraSAR-X ScanSAR data.

Highlights

  • Sea ice type distribution, especially the ratio of the multi-year ice (MYI) coverage to the seasonal ice coverage, has changed in the Arctic in recent decades

  • Sea ice classification is a method of discriminating between multi-year and seasonal ice using remote sensing data

  • The results show that the two-scale method performs well for the scenes with ice types and water with obvious differences in backscatter

Read more

Summary

Introduction

Especially the ratio of the multi-year ice (MYI) coverage to the seasonal ice coverage, has changed in the Arctic in recent decades. The MYI fraction is declining dramatically, with the seasonal ice surpassing even the MYI in the winter area coverage [1], [2]. Sea ice classification is a method of discriminating between multi-year and seasonal ice using remote sensing data. Polar regions often experience extreme weather; heavy cloud cover in summer and long periods of darkness in winter are Manuscript received. Color versions of one or more of the Figures in this paper are available online at http://ieeexplore.ieee.org

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call