Abstract

For regional environmental studies it is important to know the location of the fast ice edge which affects the coastal processes in the Arctic. The aim of this study is to develop a new automated method for fast ice delineation from SAR imagery. The method is based on a fine resolution hybrid sea ice tracking algorithm utilizing advantages of feature tracking and cross-correlation approaches. The developed method consists of three main steps: drift field retrieval at sub-kilometer scale, selection of motionless features and edge delineation. The method was tested on a time series of C-band co-polarized (HH) ENVISAT ASAR and Sentinel-1 imagery in the Laptev and East Siberian Seas. The comparison of the retrieved edges with the operational ice charts produced by the Arctic and Antarctic Research Institute (Russia) showed a good agreement between the data sets with a mean distance between the edges of <15 km. Thanks to the high density of the ice drift product, the method allows for detailed fast ice edge delineation. In addition, large stamukhas with horizontal size of tens of kilometers can be detected. The proposed method can be applied for regional fast ice mapping and large stamukhas detection to aid coastal research. Additionally, the method can serve as a tool for operational sea ice mapping.

Highlights

  • IntroductionPublisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations

  • A comparison with the operational sea ice charts showed that the developed method is capable of accurate fast ice edge delineation and detection of large stamukhas

  • The mean distance between the detected fast ice edges and the corresponding manually derived ones from the operational sea ice charts is in order of 10 km

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Summary

Introduction

Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations. Fast ice is sea ice adjacent to the coast which lacks motion for a certain period [1]. Fast ice is an important component of the Arctic coastal environment. Fast ice forms seasonally in the majority of the Arctic marginal seas. Multiyear fast ice is an exceptional phenomenon in the Arctic. Its occurrence is limited to the Canadian Archipelago [2], parts of the Taymyr

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