Abstract

In this article, we focus on developing a novel method to extract sea ice cover (i.e., discrimination/classification of sea ice and open water) using Sentinel-1 (S1) cross-polarization [vertical-horizontal (VH) or horizontal-vertical (HV)] data in extra-wide (EW) swath mode based on the support vector machine (SVM) method. The classification basis includes the S1 radar backscatter and texture features, which are calculated from S1 data using the gray level co-occurrence matrix (GLCM). Different from previous methods where appropriate samples are manually selected to train the SVM to classify sea ice and open water, we proposed a method of unsupervised generation of the training samples based on two GLCM texture features, i.e., entropy and homogeneity, that have contrasting characteristics on sea ice and open water. We eliminate the most uncertainty of selecting training samples in machine learning and achieve automatic classification of sea ice and open water by using S1 EW data. The comparisons based on a few cases show good agreements between the synthetic aperture radar (SAR)-derived sea ice cover using the proposed method and visual inspections, of which the accuracy reaches approximately 90%-95%. Besides this, compared with the analyzed sea ice cover data Ice Mapping System (IMS) based on 728 S1 EW images, the accuracy of the extracted sea ice cover by using S1 data is more than 80%.

Highlights

  • SATELLITE remote sensing is among the primary tools used to monitor polar regions where severe weather conditions present great obstacles to field research

  • We present the comparisons of the SARderived sea ice cover results with visual inspection results based on a few cases, and with the Ice Mapping System (IMS) data based on a large amount of extra wide (EW) data(728 scenes)acquired over the marginal ice zone (MIZ) in Arctic ocean

  • The two synthetic aperture radar (SAR) sensors carried by S1A and S1B have been acquiring images in wide swath (~ 400 km) HH and HV polarizations, and these sensors are dedicated to monitoring sea ice in the Arctic

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Summary

Introduction

SATELLITE remote sensing is among the primary tools used to monitor polar regions where severe weather conditions present great obstacles to field research. As one of the most important indicators of climate change in polar regions, has major impacts on the atmosphere, oceans, and terrestrialmarine ecosystem. Numerous attempts have been made to monitor sea ice in polar regions. The spaceborne radiometer (passive sensor) and scatterometer (active sensor) are two major techniques used for monitoring sea ice in polar regions. Observations have been widely explored to derive sea ice extent, concentration, and motion for operational service [1] – [4]. The spaceborne microwave radiometer yields the longest timeseries of sea ice cover in the polar regions since 1979, showing that the average Arctic Sea ice extent is declining at a rate of

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