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dc.contributor.authorRösel, Anja
dc.contributor.authorKing, Jennifer
dc.contributor.authorDoulgeris, Anthony P.
dc.contributor.authorWagner, Penelope M.
dc.contributor.authorJohansson, Malin
dc.contributor.authorGerland, Sebastian
dc.date.accessioned2018-08-14T10:47:42Z
dc.date.available2018-08-14T10:47:42Z
dc.date.issued2017-12-17
dc.description.abstractKnowledge of Arctic sea-ice conditions is of great interest for Arctic residents, as well as for commercial usage, and to study the effects of climate change. Information gained from analysis of satellite data contributes to this understanding. In the course of using in situ data in combination with remotely sensed data, the question of how representative local scale measurements are of a wider region may arise. We compare in situ total sea-ice thickness measurements from the Norwegian young sea ICE expedition in the area north of Svalbard with airborne-derived total sea-ice thickness from electromagnetic soundings. A segmented and classified synthetic aperture radar (SAR) quad-pol ALOS-2 Palsar-2 satellite scene was grouped into three simplified ice classes. The area fractions of the three classes are: 11.2% ‘thin’, 74.4% ‘level’, and 14.4% ‘deformed’. The area fractions of the simplified classes from ground- and helicopter-based measurements are comparable with those achieved from the SAR data. Thus, this study shows that there is potential for a stepwise upscaling from in situ, to airborne, to satellite data, which allow us to assess whether in situ data collected are representative of a wider region as observed by satellites.en_US
dc.descriptionSource at <a href= https://doi.org/10.1017/aog.2017.37> https://doi.org/10.1017/aog.2017.37 </a>.en_US
dc.identifier.citationRösel, A., King, J., Doulgeris, A.P., Wagner, P.M., Johansson, M. & Gerland, S. (2018). Can we extend local sea-ice measurements to satellite scale? An example from the N-ICE2015 expedition. Annals of Glaciology, 59(76), 163-172. https://doi.org/10.1017/aog.2017.37.en_US
dc.identifier.cristinIDFRIDAID 1507744
dc.identifier.doi10.1017/aog.2017.37
dc.identifier.issn0260-3055
dc.identifier.issn1727-5644
dc.identifier.urihttps://hdl.handle.net/10037/13396
dc.language.isoengen_US
dc.publisherCambridge University Pressen_US
dc.relation.journalAnnals of Glaciology
dc.relation.projectIDinfo:eu-repo/grantAgreement/RCN/NORRUSS/233896/Norway/Detection and Characterization of Anthropogenic Oil Pollution in the Barents Sea by Synthetic Aperture Radar//en_US
dc.relation.projectIDinfo:eu-repo/grantAgreement/RCN/SFI/237906/Norway/Centre for Integrated Remote Sensing and Forecasting for Arctic Operations/CIRFA/en_US
dc.rights.accessRightsopenAccessen_US
dc.subjectVDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Elektromagnetisme, akustikk, optikk: 434en_US
dc.subjectVDP::Mathematics and natural science: 400::Physics: 430::Electromagnetism, acoustics, optics: 434en_US
dc.subjectAirborne electromagnetic soundingsen_US
dc.subjectElectromagnetic inductionen_US
dc.subjectRemote sensingen_US
dc.subjectSea-iceen_US
dc.subjectSea-ice classificationen_US
dc.titleCan we extend local sea-ice measurements to satellite scale? An example from the N-ICE2015 expeditionen_US
dc.typeJournal articleen_US
dc.typeTidsskriftartikkelen_US
dc.typePeer revieweden_US


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