Sea-Ice Wintertime Lead Frequencies and Regional Characteristics in the Arctic, 2003–2015

The presence of sea-ice leads represents a key feature of the Arctic sea ice cover. Leads promote the flux of sensible and latent heat from the ocean to the cold winter atmosphere and are thereby crucial for air-sea-ice-ocean interactions. We here apply a binary segmentation procedure to identify le...

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Published in:Remote Sensing
Main Authors: Willmes, Sascha, Heinemann, Günther
Format: Article in Journal/Newspaper
Language:English
Published: MDPI 2016
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/31758/
https://oceanrep.geomar.de/id/eprint/31758/1/remotesensing-08-00004.pdf
https://doi.org/10.3390/rs8010004
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spelling ftoceanrep:oai:oceanrep.geomar.de:31758 2023-05-15T14:25:16+02:00 Sea-Ice Wintertime Lead Frequencies and Regional Characteristics in the Arctic, 2003–2015 Willmes, Sascha Heinemann, Günther 2016 text https://oceanrep.geomar.de/id/eprint/31758/ https://oceanrep.geomar.de/id/eprint/31758/1/remotesensing-08-00004.pdf https://doi.org/10.3390/rs8010004 en eng MDPI https://oceanrep.geomar.de/id/eprint/31758/1/remotesensing-08-00004.pdf Willmes, S. and Heinemann, G. (2016) Sea-Ice Wintertime Lead Frequencies and Regional Characteristics in the Arctic, 2003–2015. Open Access Remote Sensing, 8 (1). p. 4. DOI 10.3390/rs8010004 <https://doi.org/10.3390/rs8010004>. doi:10.3390/rs8010004 cc_by_4.0 info:eu-repo/semantics/openAccess Article PeerReviewed 2016 ftoceanrep https://doi.org/10.3390/rs8010004 2023-04-07T15:24:10Z The presence of sea-ice leads represents a key feature of the Arctic sea ice cover. Leads promote the flux of sensible and latent heat from the ocean to the cold winter atmosphere and are thereby crucial for air-sea-ice-ocean interactions. We here apply a binary segmentation procedure to identify leads from MODIS thermal infrared imagery on a daily time scale. The method separates identified leads into two uncertainty categories, with the high uncertainty being attributed to artifacts that arise from warm signatures of unrecognized clouds. Based on the obtained lead detections, we compute quasi-daily pan-Arctic lead maps for the months of January to April, 2003–2015. Our results highlight the marginal ice zone in the Fram Strait and Barents Sea as the primary region for lead activity. The spatial distribution of the average pan-Arctic lead frequencies reveals, moreover, distinct patterns of predominant fracture zones in the Beaufort Sea and along the shelf-breaks, mainly in the Siberian sector of the Arctic Ocean as well as the well-known polynya and fast-ice locations. Additionally, a substantial inter-annual variability of lead occurrences in the Arctic is indicated. Article in Journal/Newspaper Arctic Arctic Arctic Ocean Barents Sea Beaufort Sea Fram Strait Sea ice OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Arctic Arctic Ocean Barents Sea Remote Sensing 8 1 4
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
description The presence of sea-ice leads represents a key feature of the Arctic sea ice cover. Leads promote the flux of sensible and latent heat from the ocean to the cold winter atmosphere and are thereby crucial for air-sea-ice-ocean interactions. We here apply a binary segmentation procedure to identify leads from MODIS thermal infrared imagery on a daily time scale. The method separates identified leads into two uncertainty categories, with the high uncertainty being attributed to artifacts that arise from warm signatures of unrecognized clouds. Based on the obtained lead detections, we compute quasi-daily pan-Arctic lead maps for the months of January to April, 2003–2015. Our results highlight the marginal ice zone in the Fram Strait and Barents Sea as the primary region for lead activity. The spatial distribution of the average pan-Arctic lead frequencies reveals, moreover, distinct patterns of predominant fracture zones in the Beaufort Sea and along the shelf-breaks, mainly in the Siberian sector of the Arctic Ocean as well as the well-known polynya and fast-ice locations. Additionally, a substantial inter-annual variability of lead occurrences in the Arctic is indicated.
format Article in Journal/Newspaper
author Willmes, Sascha
Heinemann, Günther
spellingShingle Willmes, Sascha
Heinemann, Günther
Sea-Ice Wintertime Lead Frequencies and Regional Characteristics in the Arctic, 2003–2015
author_facet Willmes, Sascha
Heinemann, Günther
author_sort Willmes, Sascha
title Sea-Ice Wintertime Lead Frequencies and Regional Characteristics in the Arctic, 2003–2015
title_short Sea-Ice Wintertime Lead Frequencies and Regional Characteristics in the Arctic, 2003–2015
title_full Sea-Ice Wintertime Lead Frequencies and Regional Characteristics in the Arctic, 2003–2015
title_fullStr Sea-Ice Wintertime Lead Frequencies and Regional Characteristics in the Arctic, 2003–2015
title_full_unstemmed Sea-Ice Wintertime Lead Frequencies and Regional Characteristics in the Arctic, 2003–2015
title_sort sea-ice wintertime lead frequencies and regional characteristics in the arctic, 2003–2015
publisher MDPI
publishDate 2016
url https://oceanrep.geomar.de/id/eprint/31758/
https://oceanrep.geomar.de/id/eprint/31758/1/remotesensing-08-00004.pdf
https://doi.org/10.3390/rs8010004
geographic Arctic
Arctic Ocean
Barents Sea
geographic_facet Arctic
Arctic Ocean
Barents Sea
genre Arctic
Arctic
Arctic Ocean
Barents Sea
Beaufort Sea
Fram Strait
Sea ice
genre_facet Arctic
Arctic
Arctic Ocean
Barents Sea
Beaufort Sea
Fram Strait
Sea ice
op_relation https://oceanrep.geomar.de/id/eprint/31758/1/remotesensing-08-00004.pdf
Willmes, S. and Heinemann, G. (2016) Sea-Ice Wintertime Lead Frequencies and Regional Characteristics in the Arctic, 2003–2015. Open Access Remote Sensing, 8 (1). p. 4. DOI 10.3390/rs8010004 <https://doi.org/10.3390/rs8010004>.
doi:10.3390/rs8010004
op_rights cc_by_4.0
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.3390/rs8010004
container_title Remote Sensing
container_volume 8
container_issue 1
container_start_page 4
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