Investigating High-Resolution AMSR2 Sea Ice Concentrations during the February 2013 Fracture Event in the Beaufort Sea

Leads with a length on the order of 1000 km occurred in the Beaufort Sea in February 2013. These leads can be observed in Moderate Resolution Imaging Spectroradiometer (MODIS) images under predominantly clear sky conditions. Sea ice concentrations (SIC) derived from the Advanced Microwave Scanning R...

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Main Authors: Alexander Beitsch, Lars Kaleschke, Stefan Kern
Format: Article
Language:English
Published: MDPI AG 2014-04-01
Series:Remote Sensing
Subjects:
Online Access:http://www.mdpi.com/2072-4292/6/5/3841
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spelling doaj-5edccd889e16427282af5d8db137945c2020-11-25T00:52:19ZengMDPI AGRemote Sensing2072-42922014-04-01653841385610.3390/rs6053841rs6053841Investigating High-Resolution AMSR2 Sea Ice Concentrations during the February 2013 Fracture Event in the Beaufort SeaAlexander Beitsch0Lars Kaleschke1Stefan Kern2Institute of Oceanography, University of Hamburg, Bundesstraße 53, 20146 Hamburg, GermanyInstitute of Oceanography, University of Hamburg, Bundesstraße 53, 20146 Hamburg, GermanyIntegrated Climate Data Center (ICDC), Center for Earth System Research and Sustainability (CEN), University of Hamburg , Grindelberg 5, 20144 Hamburg, GermanyLeads with a length on the order of 1000 km occurred in the Beaufort Sea in February 2013. These leads can be observed in Moderate Resolution Imaging Spectroradiometer (MODIS) images under predominantly clear sky conditions. Sea ice concentrations (SIC) derived from the Advanced Microwave Scanning Radiometer 2 (AMSR2) using the Bootstrap (BST) algorithm fail to show the lead occurrences, as is visible in the MODIS images. In contrast, SIC derived from AMSR2 using the Arctic Radiation and Turbulence Interaction Study (ARTIST) sea ice algorithm (ASI) reveal the lead structure, due to the higher spatial resolution possible when using 89-GHz channel data. The ASI SIC are calculated from brightness temperatures interpolated on three different grids with resolutions of 3.125 km (ASI-3k), 6.25 km (ASI-6k) and 12.5 km (ASI-12k) to investigate the effect of the spatial resolution. Single-swath data is used to study the effect of temporal sampling in comparison to daily averages. For a region of interest in the Beaufort Sea, BST and ASI-3k show area-averaged SIC of 97%±0.7% and 93%±7.0%, respectively. For ASI-6k, the area-averaged SIC are similar to ASI-3k, while ASI-12k data show more agreement with BST. Visual comparison with MODIS True Color imagery exhibits good agreement with ASI-3k. In particular, ASI-3k are able to reproduce lead structure and size in the sea ice cover, which are not or are less visible in the other SIC data. The results will be valuable for selecting a SIC data product for studies of the interaction between ocean, ice, and atmosphere in the polar regions.http://www.mdpi.com/2072-4292/6/5/3841AMSR2passive-microwave remote sensingsea ice concentrationARTIST sea ice algorithm
collection DOAJ
language English
format Article
sources DOAJ
author Alexander Beitsch
Lars Kaleschke
Stefan Kern
spellingShingle Alexander Beitsch
Lars Kaleschke
Stefan Kern
Investigating High-Resolution AMSR2 Sea Ice Concentrations during the February 2013 Fracture Event in the Beaufort Sea
Remote Sensing
AMSR2
passive-microwave remote sensing
sea ice concentration
ARTIST sea ice algorithm
author_facet Alexander Beitsch
Lars Kaleschke
Stefan Kern
author_sort Alexander Beitsch
title Investigating High-Resolution AMSR2 Sea Ice Concentrations during the February 2013 Fracture Event in the Beaufort Sea
title_short Investigating High-Resolution AMSR2 Sea Ice Concentrations during the February 2013 Fracture Event in the Beaufort Sea
title_full Investigating High-Resolution AMSR2 Sea Ice Concentrations during the February 2013 Fracture Event in the Beaufort Sea
title_fullStr Investigating High-Resolution AMSR2 Sea Ice Concentrations during the February 2013 Fracture Event in the Beaufort Sea
title_full_unstemmed Investigating High-Resolution AMSR2 Sea Ice Concentrations during the February 2013 Fracture Event in the Beaufort Sea
title_sort investigating high-resolution amsr2 sea ice concentrations during the february 2013 fracture event in the beaufort sea
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2014-04-01
description Leads with a length on the order of 1000 km occurred in the Beaufort Sea in February 2013. These leads can be observed in Moderate Resolution Imaging Spectroradiometer (MODIS) images under predominantly clear sky conditions. Sea ice concentrations (SIC) derived from the Advanced Microwave Scanning Radiometer 2 (AMSR2) using the Bootstrap (BST) algorithm fail to show the lead occurrences, as is visible in the MODIS images. In contrast, SIC derived from AMSR2 using the Arctic Radiation and Turbulence Interaction Study (ARTIST) sea ice algorithm (ASI) reveal the lead structure, due to the higher spatial resolution possible when using 89-GHz channel data. The ASI SIC are calculated from brightness temperatures interpolated on three different grids with resolutions of 3.125 km (ASI-3k), 6.25 km (ASI-6k) and 12.5 km (ASI-12k) to investigate the effect of the spatial resolution. Single-swath data is used to study the effect of temporal sampling in comparison to daily averages. For a region of interest in the Beaufort Sea, BST and ASI-3k show area-averaged SIC of 97%±0.7% and 93%±7.0%, respectively. For ASI-6k, the area-averaged SIC are similar to ASI-3k, while ASI-12k data show more agreement with BST. Visual comparison with MODIS True Color imagery exhibits good agreement with ASI-3k. In particular, ASI-3k are able to reproduce lead structure and size in the sea ice cover, which are not or are less visible in the other SIC data. The results will be valuable for selecting a SIC data product for studies of the interaction between ocean, ice, and atmosphere in the polar regions.
topic AMSR2
passive-microwave remote sensing
sea ice concentration
ARTIST sea ice algorithm
url http://www.mdpi.com/2072-4292/6/5/3841
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