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: Hoi Ming Lam, Gunnar Spreen, Georg Heygster, Christian Melsheimer, Neal W. Young
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2018
Subjects:
Online Access:https://doi.org/10.1017/aog.2018.1
https://doaj.org/article/9dfc29868e3746f6b961dba358477bfe
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spelling ftdoajarticles:oai:doaj.org/article:9dfc29868e3746f6b961dba358477bfe 2023-05-15T13:29:36+02:00 Erroneous sea-ice concentration retrieval in the East Antarctic Hoi Ming Lam Gunnar Spreen Georg Heygster Christian Melsheimer Neal W. Young 2018-07-01T00:00:00Z https://doi.org/10.1017/aog.2018.1 https://doaj.org/article/9dfc29868e3746f6b961dba358477bfe EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0260305518000010/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2018.1 0260-3055 1727-5644 https://doaj.org/article/9dfc29868e3746f6b961dba358477bfe Annals of Glaciology, Vol 59, Pp 201-212 (2018) atmosphere/ice/ocean interactions remote sensing sea ice sea-ice geophysics Meteorology. Climatology QC851-999 article 2018 ftdoajarticles https://doi.org/10.1017/aog.2018.1 2023-03-12T01:31:57Z 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 Directory of Open Access Journals: DOAJ Articles Antarctic The Antarctic Annals of Glaciology 59 76pt2 201 212
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic atmosphere/ice/ocean interactions
remote sensing
sea ice
sea-ice geophysics
Meteorology. Climatology
QC851-999
spellingShingle atmosphere/ice/ocean interactions
remote sensing
sea ice
sea-ice geophysics
Meteorology. Climatology
QC851-999
Hoi Ming Lam
Gunnar Spreen
Georg Heygster
Christian Melsheimer
Neal W. Young
Erroneous sea-ice concentration retrieval in the East Antarctic
topic_facet atmosphere/ice/ocean interactions
remote sensing
sea ice
sea-ice geophysics
Meteorology. Climatology
QC851-999
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 Hoi Ming Lam
Gunnar Spreen
Georg Heygster
Christian Melsheimer
Neal W. Young
author_facet Hoi Ming Lam
Gunnar Spreen
Georg Heygster
Christian Melsheimer
Neal W. Young
author_sort Hoi Ming Lam
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 Cambridge University Press
publishDate 2018
url https://doi.org/10.1017/aog.2018.1
https://doaj.org/article/9dfc29868e3746f6b961dba358477bfe
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_source Annals of Glaciology, Vol 59, Pp 201-212 (2018)
op_relation https://www.cambridge.org/core/product/identifier/S0260305518000010/type/journal_article
https://doaj.org/toc/0260-3055
https://doaj.org/toc/1727-5644
doi:10.1017/aog.2018.1
0260-3055
1727-5644
https://doaj.org/article/9dfc29868e3746f6b961dba358477bfe
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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