Erroneous sea-ice concentration retrieval in the East Antarctic

Large discrepancies have been observed between satellite-derived sea-ice concentrations(IC) from passive microwave remote sensing and those derived from optical images at several locations in the East Antarctic, between February and April 2014. These artefacts, that resemble polynyas in the IC maps,...

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Published in:Annals of Glaciology
Main Authors: Lam, HM, Spreen, G, Heygster, G, Melsheimer, C, Young, NW
Format: Article in Journal/Newspaper
Language:English
Published: Int Glaciol Soc 2018
Subjects:
Online Access:https://eprints.utas.edu.au/29952/
https://eprints.utas.edu.au/29952/1/131760%20-%20Erroneous%20sea-ice%20concentration%20retrieval%20in%20the%20East%20Antarctic.pdf
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spelling ftunivtasmania:oai:eprints.utas.edu.au:29952 2023-05-15T13:29:44+02:00 Erroneous sea-ice concentration retrieval in the East Antarctic Lam, HM Spreen, G Heygster, G Melsheimer, C Young, NW 2018 application/pdf https://eprints.utas.edu.au/29952/ https://eprints.utas.edu.au/29952/1/131760%20-%20Erroneous%20sea-ice%20concentration%20retrieval%20in%20the%20East%20Antarctic.pdf en eng Int Glaciol Soc https://eprints.utas.edu.au/29952/1/131760%20-%20Erroneous%20sea-ice%20concentration%20retrieval%20in%20the%20East%20Antarctic.pdf Lam, HM, Spreen, G, Heygster, G, Melsheimer, C and Young, NW 2018 , 'Erroneous sea-ice concentration retrieval in the East Antarctic' , Annals of Glaciology, vol. 59, no. 76pt2 , pp. 201-212 , doi:10.1017/aog.2018.1 <http://dx.doi.org/10.1017/aog.2018.1>. atmosphere/ice/ocean interactions remote sensing sea ice sea-ice geophysics Article PeerReviewed 2018 ftunivtasmania https://doi.org/10.1017/aog.2018.1 2021-09-13T22:19:30Z Large discrepancies have been observed between satellite-derived sea-ice concentrations(IC) from passive microwave remote sensing and those derived from optical images at several locations in the East Antarctic, between February and April 2014. These artefacts, that resemble polynyas in the IC maps, appear in areas where optical satellite data show that there is landfast sea ice. The IC datasets and the corresponding retrieval algorithms are investigated together with microwave brightness temperature, air temperature, snowfall and bathymetry to understand the failure of the IC retrieval. The artefacts are the result of the application of weather filters in retrieval algorithms. These filters use the 37 and 19 GHz channels to correct for atmospheric effects on the retrieval. These channels show significant departures from typical ranges when the artefacts occur. A melt–refreeze cycle with associated snow metamorphism is proposed as the most likely cause. Together, the areas of the artefacts account for up to 0.5% of the Antarctic sea-ice area and thus cause a bias in sea-IC time series. In addition, erroneous sea ICs can adversely affect shipping operations. Article in Journal/Newspaper Annals of Glaciology Antarc* Antarctic Sea ice University of Tasmania: UTas ePrints Antarctic The Antarctic Annals of Glaciology 59 76pt2 201 212
institution Open Polar
collection University of Tasmania: UTas ePrints
op_collection_id ftunivtasmania
language English
topic atmosphere/ice/ocean interactions
remote sensing
sea ice
sea-ice geophysics
spellingShingle atmosphere/ice/ocean interactions
remote sensing
sea ice
sea-ice geophysics
Lam, HM
Spreen, G
Heygster, G
Melsheimer, C
Young, NW
Erroneous sea-ice concentration retrieval in the East Antarctic
topic_facet atmosphere/ice/ocean interactions
remote sensing
sea ice
sea-ice geophysics
description Large discrepancies have been observed between satellite-derived sea-ice concentrations(IC) from passive microwave remote sensing and those derived from optical images at several locations in the East Antarctic, between February and April 2014. These artefacts, that resemble polynyas in the IC maps, appear in areas where optical satellite data show that there is landfast sea ice. The IC datasets and the corresponding retrieval algorithms are investigated together with microwave brightness temperature, air temperature, snowfall and bathymetry to understand the failure of the IC retrieval. The artefacts are the result of the application of weather filters in retrieval algorithms. These filters use the 37 and 19 GHz channels to correct for atmospheric effects on the retrieval. These channels show significant departures from typical ranges when the artefacts occur. A melt–refreeze cycle with associated snow metamorphism is proposed as the most likely cause. Together, the areas of the artefacts account for up to 0.5% of the Antarctic sea-ice area and thus cause a bias in sea-IC time series. In addition, erroneous sea ICs can adversely affect shipping operations.
format Article in Journal/Newspaper
author Lam, HM
Spreen, G
Heygster, G
Melsheimer, C
Young, NW
author_facet Lam, HM
Spreen, G
Heygster, G
Melsheimer, C
Young, NW
author_sort Lam, HM
title Erroneous sea-ice concentration retrieval in the East Antarctic
title_short Erroneous sea-ice concentration retrieval in the East Antarctic
title_full Erroneous sea-ice concentration retrieval in the East Antarctic
title_fullStr Erroneous sea-ice concentration retrieval in the East Antarctic
title_full_unstemmed Erroneous sea-ice concentration retrieval in the East Antarctic
title_sort erroneous sea-ice concentration retrieval in the east antarctic
publisher Int Glaciol Soc
publishDate 2018
url https://eprints.utas.edu.au/29952/
https://eprints.utas.edu.au/29952/1/131760%20-%20Erroneous%20sea-ice%20concentration%20retrieval%20in%20the%20East%20Antarctic.pdf
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Annals of Glaciology
Antarc*
Antarctic
Sea ice
genre_facet Annals of Glaciology
Antarc*
Antarctic
Sea ice
op_relation https://eprints.utas.edu.au/29952/1/131760%20-%20Erroneous%20sea-ice%20concentration%20retrieval%20in%20the%20East%20Antarctic.pdf
Lam, HM, Spreen, G, Heygster, G, Melsheimer, C and Young, NW 2018 , 'Erroneous sea-ice concentration retrieval in the East Antarctic' , Annals of Glaciology, vol. 59, no. 76pt2 , pp. 201-212 , doi:10.1017/aog.2018.1 <http://dx.doi.org/10.1017/aog.2018.1>.
op_doi https://doi.org/10.1017/aog.2018.1
container_title Annals of Glaciology
container_volume 59
container_issue 76pt2
container_start_page 201
op_container_end_page 212
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