Abstract

The Northwest Passage (NWP) in the Arctic is usually covered with hazardous multi-year ice (MYI) and seasonal first-year ice (FYI) in winter, with possible thin ice and open-water areas during transition seasons. Ice classification is important for both marine navigation and climate change studies. Satellite-based Synthetic Aperture Radar (SAR) systems have shown advantages of retrieving this information. Operational ice mapping relies on visual analysis of SAR images along with ancillary data. However, these maps estimate ice types and concentrations within large-size polygons of a few tens or hundreds of kilometers, which are subjectively identified and selected by analysts. This study aims at developing an automated algorithm to identify individual MYI floes from SAR images then classify the rest of the image as FYI and other ice types. The algorithm identifies the MYI floes using extended-maximum operator, morphological image processing, and a few geometrical features. Classifying the rest of the image uses texture and neural network model. The input data is a set of Sentinel-1 A/B Extended Wide (EW) mode images, acquired between September and March 2016–2019. Although the overall accuracy (for all type classification) from the new method scored 93.26%, the accuracy from using the texture classifier only was 75.81%. The kappa coefficient from the former was higher than the latter by 0.25. Compared with the operational ice charts from the Canadian Ice Service, ice type maps from the new method show better distribution of MYI at the fine scale of individual floes. Comparison against MYI concentration from two automated algorithms that use a combination of coarse-resolution passive and active microwave data also confirms the advantage of resolving MYI floes from the fine-resolution SAR.

Highlights

  • The Northwest Passage (NWP) connects the eastern Arctic to the Chukchi Sea, passing through the Canadian Arctic Archipelago (CAA)

  • This channel is a pathway of sea ice from the central Arctic, but it does not end at an open sea

  • The TPO method overestimates the areal extent of the multi-year ice (MYI) because the texture of the surrounding first-year ice (FYI) is very similar to that of MYI

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Summary

Introduction

The Northwest Passage (NWP) connects the eastern Arctic to the Chukchi Sea, passing through the Canadian Arctic Archipelago (CAA). With the recent decline of Arctic ice cover and the replenishment of MYI by thinner and less navigational-hazard first-year ice (FYI) [1,2,3], it is predicted that the NWP may open for marine navigation in future summers if it becomes MYI-free. This will provide an alternative shipping route between Asia and Europe [4,5]. This emphasizes the importance of monitoring sea ice type in the NWP

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