Abstract

In recent years, much attention has been paid to the behavior of passive microwave sea ice concentration (SIC) products for marginal ice zones. Based on the definition of ice edges from ship observations, we identified pseudo-ship observations (PSO) and generated PSO ice edges from twelve cloud-free moderate-resolution imaging spectroradiometer (MODIS) images. Two SIC products of the advanced microwave scanning radiometer 2 (AMSR2) were compared at the PSO ice edges: ARTIST (arctic radiation and turbulence interaction study) sea ice (ASI-SIC) and bootstrap (BST-SIC). The mean values of ASI-SIC pixels located at ice edges were 10.5% and 10.3% for the Arctic and the Antarctic, respectively, and are below the commonly applied 15% threshold, whereas the mean values of corresponding BST-SIC pixels were 23.6% and 27.3%, respectively. The mean values of both ASI-SIC and BST-SIC were lower in summer than in winter. The spatial gaps among the 15% ASI-SIC ice edge, the 15% BST-SIC ice edge and the PSO ice edge were mostly within 35 km, whereas the 15% ASI-SIC ice edge matched better with the PSO ice edge. Results also show that the ice edges were located in the thin ice region, with a mean ice thickness of around 5–8 cm. We conclude that the 15% threshold well determines the ice edge from passive microwave SIC in both the Arctic and the Antarctic.

Highlights

  • Sea ice, as a major component of the cryosphere, significantly influences the polar and global climate [1]

  • Ice thickness at the edges was extracted from SMOS images to examine their ability to define “edge” from the thickness perspective

  • This study compared ASI-sea ice concentration (SIC) with BST-SIC at the pseudo-ship observations (PSO) ice edge extracted from moderate-resolution imaging spectroradiometer (MODIS) images

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Summary

Introduction

As a major component of the cryosphere, significantly influences the polar and global climate [1]. The decreasing sea ice coverage is one of the most obvious indicators of global warming, which can be estimated from the retreat of sea ice edges [4,5]. Satellite passive microwave data, which are weather- and daylight-independent, have been used to identify trends and variability in ice extent in the polar region as well as in locating ice edges [6]. Satellite launches are accompanied by the development of passive microwave SIC algorithms, such as the NASA-team (NT), the enhanced NASA-team (NT2), BST and ASI. ASI and BST algorithms have been applied on AMSR2 and the daily ASI-SIC and BST-SIC map based on AMSR2 has been accessible since August 2012

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