Abstract

Efficient and accurate segmentation of sea ice floes from high-resolution optical (HRO) remote sensing images is crucial for understanding of sea ice evolutions and climate changes, especially in coping with the large data volume. Existing methods suffer from noise interference and the mixture of water and ice caused high segmentation error and less robustness. In this article, we propose a novel sea ice floe segmentation algorithm from HRO images based on texture-sensitive superpixeling and two-stage thresholding. First, sparse components are extracted from the HRO images using the robust principal component analysis (RPCA), and noise is removed by the bilateral filter. The enhanced image is obtained by combining the low-rank matrix and the sparse components. Second, a texture-sensitive simple linear iterative clustering (SLIC) superpixel algorithm is introduced for presegmentation of the enhanced HRO image. Third, a learning-based adaptive thresholding in the two stages is employed to generate the refined segmentation from the derived superpixels blocks. The efficacy of the proposed method is validated on two HRO images using visual assessment, quantitative evaluation (with seven metrics), and histogram comparison. The superior performance of the proposed method has demonstrated its efficacy for sea ice floe segmentation.

Highlights

  • S EA ice floe segmentation is an important topic in remote sensing

  • We aim to apply superpixel for sea ice floe segmentation from high-resolution optical (HRO) images, where the challenges are how to deal with the low contrast areas of mixed ice and water and accurate segmentation of touching floes of arbitrary sizes and shapes

  • Sparse components are extracted from the high-resolution remote sensing image by using robust principal component analysis (RPCA), and the bilateral filter is used on it to remove noise

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Summary

Introduction

S EA ice floe segmentation is an important topic in remote sensing. With regular data provided covering, an increasingly wide area, and a relatively high temporal resolution, various satelliteborne sensors are used in sea ice applications. Scatterometers can provide a fast and noncontact method for topography assessment, it suffers from a low spatial resolution and, can only detect large sea ice floes or icebergs. SAR suffers from severe speckle noise and limited spatial resolution; it is difficult to detect small ice floes [3]. With the advancement of satellite technology, high-resolution optical (HRO) imagery has provided another alternative solution, as it enables accurate detection of the textures, shapes, and edges of the sea ice floes [4]

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