Vis enkel innførsel

dc.contributor.authorRabault, Jean
dc.contributor.authorTaelman, Catherine Cecilia A
dc.contributor.authorIdzanovic, Martina
dc.contributor.authorHope, Gaute
dc.contributor.authorNose, Takehiko
dc.contributor.authorKristoffersen, Yngve
dc.contributor.authorJensen, Atle
dc.contributor.authorBreivik, Øyvind
dc.contributor.authorBryhni, Helge
dc.contributor.authorHoppmann, Mario
dc.contributor.authorDemchev, Denis
dc.contributor.authorKorosov, Anton
dc.contributor.authorJohansson, Anna Malin Kristin
dc.contributor.authorEltoft, Torbjørn
dc.contributor.authorDagestad, Knut-Frode
dc.contributor.authorRöhrs, Johannes
dc.contributor.authorEriksson, Leif
dc.contributor.authorDurán Moro, Marina
dc.contributor.authorRikardsen, Edel
dc.contributor.authorWaseda, Takuji
dc.contributor.authorKodaira, Tsubasa
dc.contributor.authorLohse, Johannes Philipp
dc.contributor.authorDesjonquères, Thibault
dc.contributor.authorOlsen, Sveinung Viggo
dc.contributor.authorGundersen, Olav
dc.contributor.authorMartins de Aguiar, Victor Cesar
dc.contributor.authorKarlsen, Truls Thorsen
dc.contributor.authorBabanin, Alexander V.
dc.contributor.authorVoermans, Joey J.
dc.contributor.authorPark, Jeong-Won
dc.contributor.authorMüller, Malte
dc.date.accessioned2025-01-08T10:20:45Z
dc.date.available2025-01-08T10:20:45Z
dc.date.issued2024-12-21
dc.description.abstractSea ice is a key element of the global Earth system, with a major impact on global climate and regional weather. Unfortunately, accurate sea ice modeling is challenging due to the diversity and complexity of underlying physics happening there, and a relative lack of ground truth observations. This is especially true for the Marginal Ice Zone (MIZ), which is the area where sea ice is affected by incoming ocean waves. Waves contribute to making the area dynamic, and due to the low survival time of the buoys deployed there, the MIZ is challenging to monitor. In 2022-2023, we released 79 OpenMetBuoys (OMBs) around Svalbard, both in the MIZ and the ocean immediately outside of it. OMBs are affordable enough to be deployed in large number, and gather information about drift (GNSS position) and waves (1-dimensional elevation spectrum). This provides data focusing on the area around Svalbard with unprecedented spatial and temporal resolution. We expect that this will allow to perform validation and calibration of ice models and remote sensing algorithms.en_US
dc.identifier.citationRabault, Taelman, Idzanovic, Hope, Nose, Kristoffersen, Jensen, Breivik, Bryhni, Hoppmann, Demchev, Korosov, Johansson, Eltoft, Dagestad, Röhrs, Eriksson, Durán Moro, Rikardsen, Waseda, Kodaira, Lohse, Desjonquères, Olsen, Gundersen, Martins de Aguiar, Karlsen, Babanin, Voermans, Park, Müller. A position and wave spectra dataset of Marginal Ice Zone dynamics collected around Svalbard in 2022 and 2023. Scientific Data. 2024en_US
dc.identifier.cristinIDFRIDAID 2333445
dc.identifier.doi10.1038/s41597-024-04281-1
dc.identifier.issn2052-4463
dc.identifier.urihttps://hdl.handle.net/10037/36110
dc.language.isoengen_US
dc.publisherSpringer Natureen_US
dc.relation.journalScientific Data
dc.relation.projectIDNorges forskningsråd: 276730en_US
dc.relation.projectIDNorges forskningsråd: 237906en_US
dc.relation.projectIDNorges forskningsråd: 303411en_US
dc.relation.projectIDNorges forskningsråd: 301450en_US
dc.rights.accessRightsopenAccessen_US
dc.rights.holderCopyright 2024 The Author(s)en_US
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/4.0en_US
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0)en_US
dc.titleA position and wave spectra dataset of Marginal Ice Zone dynamics collected around Svalbard in 2022 and 2023en_US
dc.type.versionpublishedVersionen_US
dc.typeJournal articleen_US
dc.typeTidsskriftartikkelen_US
dc.typePeer revieweden_US


Tilhørende fil(er)

Thumbnail

Denne innførselen finnes i følgende samling(er)

Vis enkel innførsel

Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0)
Med mindre det står noe annet, er denne innførselens lisens beskrevet som Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0)