Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/14994
DC FieldValueLanguage
dc.date.accessioned2021-12-02T11:04:06Z-
dc.date.available2021-12-02T11:04:06Z-
dc.date.issued2021-
dc.identifier.urihttp://hdl.handle.net/2122/14994-
dc.description.abstractThe article presents a methodology for examining a temporal sequence of synthetic aperture radar (SAR) images, as applied to the detection of the A-68 iceberg and its drifting trajectory. Using an improved image processing scheme, the analysis covers a period of eighteen months and makes use of a set of Sentinel-1 images. A-68 iceberg calved from the Larsen C ice shelf in July 2017 and is one of the largest icebergs observed by remote sensing on record. After the calving, there was only a modest decrease in the area (about 1%) in the first six months. It has been drifting along the east coast of the Antarctic Peninsula, and is expected to continue its path for more than a decade. It is important to track the huge A-68 iceberg to retrieve information on the physics of iceberg dynamics and for maritime security reasons. Two relevant problems are addressed by the image processing scheme presented here: (a) How to achieve quasi-automatic analysis using a fuzzy logic approach to image contrast enhancement, and (b) The use of ferromagnetic concepts to define a stochastic segmentation. The Ising equation is used to model the energy function of the process, and the segmentation is the result of a stochastic minimization.en_US
dc.language.isoEnglishen_US
dc.publisher.nameMDPIen_US
dc.relation.ispartofRemote Sensingen_US
dc.relation.ispartofseries/13(2021)en_US
dc.titleOn the Detection and Long-Term Path Visualisation of A-68 Icebergen_US
dc.typearticleen
dc.description.statusPublisheden_US
dc.description.pagenumber460en_US
dc.identifier.doi10.3390/rs13030460en_US
dc.description.obiettivoSpecifico5A. Ricerche polari e paleoclimaen_US
dc.description.journalTypeJCR Journalen_US
dc.relation.issn2072-4292en_US
dc.contributor.authorLopez-Lopez, Ludwin-
dc.contributor.authorParmiggiani, Flavio-
dc.contributor.authorMoctezuma-Flores, Miguel-
dc.contributor.authorGuerrieri, Lorenzo-
dc.contributor.departmentFacultad de Ingenieria, Universidad Nacional Autonoma de Mexicoen_US
dc.contributor.departmentCNRen_US
dc.contributor.departmentFacultad de Ingenieria, Universidad Nacional Autonoma de Mexicoen_US
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen_US
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptFacultad de Ingenieria, Universidad Nacional Autonoma de Mexico-
crisitem.author.deptCNR-
crisitem.author.deptFacultad de Ingenieria, Universidad Nacional Autonoma de Mexico-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.orcid0000-0001-7090-1291-
crisitem.author.orcid0000-0002-6046-2421-
crisitem.author.orcid0000-0003-1894-5048-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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