Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/37628
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dc.contributor.authorEvans, Ben Richarden_UK
dc.contributor.authorLowe, Alanen_UK
dc.contributor.authorCrawford, Annaen_UK
dc.contributor.authorFleming, Andrewen_UK
dc.contributor.authorHosking, J Scotten_UK
dc.date.accessioned2025-12-03T01:08:27Z-
dc.date.available2025-12-03T01:08:27Z-
dc.date.issued2025-07-07en_UK
dc.identifier.urihttp://hdl.handle.net/1893/37628-
dc.description.abstractTabular icebergs calve from ice shelves and glaciers in Antarctica, Greenland, and northern Ellesmere Island. These ‘ice islands’, as they are referred to in the Arctic, drift, melt, and fragment, contributing fresh water and nutrients to the ocean, influencing circulation, carbon cycling and biodiversity in ways that remain poorly understood. Icebergs also pose risks to shipping, and maritime infrastructure. Improved understanding of iceberg drift and fragmentation will reduce uncertainties in climate simulations and operational hazards. This study presents the first comprehensively validated, scalable iceberg tracking approach and the first that is capable of reconstructing iceberg ‘lineages’ (here used to describe life histories including sources, where that source is a larger iceberg) through fragmentation events. This method enables a comprehensive reconstruction of iceberg paths from calving to their eventual disintegration, allowing for monitoring and source attribution across their life cycle. We propose CryoTrack, an unsupervised approach based on iceberg geometry that is agnostic to data source or delineation method. The system requires only vector outlines. Initially, icebergs are linked across timesteps when their shapes remain similar, forming ‘tracklets’. When significant shape changes occur, fragmented ‘child’ icebergs are linked to their ‘parents’ using a fuzzy geometric assembly method based on dynamic time warping, akin to assembling a jigsaw puzzle without image data. This approach reconstructs full iceberg lineages back to their calving origin. We evaluate system performance using manually tracked iceberg outlines in the Canadian Arctic. Standard tracking metrics and custom iceberg specific metrics assess its accuracy in scientific and operational contexts. Our approach achieves excellent tracking of icebergs with an overall tracking accuracy of 0.98 and 94 % of iceberg area are correctly linked to source when icebergs are last observed. This system contributes to the need for scalable iceberg monitoring. It enhances understanding of iceberg behaviours, impacts, and fragmentation, supporting process based and data driven predictive modelling for environmental and operational applications.en_UK
dc.language.isoenen_UK
dc.publisherEuropean Geosciences Unionen_UK
dc.relationEvans BR, Lowe A, Crawford A, Fleming A & Hosking JS (2025) Icebergs, jigsaw puzzles and genealogy: Automated multi-generational iceberg tracking and lineage reconstruction. <i>The Cryosphere Discussions</i>. https://doi.org/10.5194/egusphere-2025-2886en_UK
dc.rights© Author(s) 2025. This work is distributed under the Creative Commons Attribution 4.0 License.en_UK
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/en_UK
dc.titleIcebergs, jigsaw puzzles and genealogy: Automated multi-generational iceberg tracking and lineage reconstructionen_UK
dc.typeJournal Articleen_UK
dc.identifier.doi10.5194/egusphere-2025-2886en_UK
dc.citation.jtitleCryosphere Discussionsen_UK
dc.citation.issn1994-0440en_UK
dc.citation.issn1994-0432en_UK
dc.citation.peerreviewedUnrefereeden_UK
dc.type.statusSMUR - Submitted Manuscript Under Reviewen_UK
dc.contributor.funderBritish Antarctic Surveyen_UK
dc.contributor.funderEngineering and Physical Sciences Research Councilen_UK
dc.author.emailanna.crawford@stir.ac.uken_UK
dc.citation.date07/07/2025en_UK
dc.contributor.affiliationBritish Antarctic Surveyen_UK
dc.contributor.affiliationAlan Turing Instituteen_UK
dc.contributor.affiliationBiological and Environmental Sciencesen_UK
dc.contributor.affiliationBritish Antarctic Surveyen_UK
dc.contributor.affiliationBritish Antarctic Surveyen_UK
dc.identifier.wtid2209361en_UK
dc.contributor.orcid0000-0003-0643-526Xen_UK
dc.contributor.orcid0000-0003-3620-1130en_UK
dc.date.accepted2025-07-07en_UK
dcterms.dateAccepted2025-07-07en_UK
dc.date.filedepositdate2025-11-19en_UK
rioxxterms.apcnot requireden_UK
rioxxterms.versionSMURen_UK
local.rioxx.authorEvans, Ben Richard|0000-0003-0643-526Xen_UK
local.rioxx.authorLowe, Alan|en_UK
local.rioxx.authorCrawford, Anna|0000-0003-3620-1130en_UK
local.rioxx.authorFleming, Andrew|en_UK
local.rioxx.authorHosking, J Scott|en_UK
local.rioxx.projectProject ID unknown|Engineering and Physical Sciences Research Council|http://dx.doi.org/10.13039/501100000266en_UK
local.rioxx.projectProject ID unknown|British Antarctic Survey|http://dx.doi.org/10.13039/501100007849en_UK
local.rioxx.freetoreaddate2025-12-01en_UK
local.rioxx.licencehttp://creativecommons.org/licenses/by/4.0/|2025-12-01|en_UK
local.rioxx.filenameegusphere-2025-2886.pdfen_UK
local.rioxx.filecount1en_UK
local.rioxx.source1994-0440en_UK
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