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dc.contributor.authorRicker, Robert
dc.contributor.authorFons, Steven
dc.contributor.authorJutila, Arttu
dc.contributor.authorHutter, Nils
dc.contributor.authorDuncan, Kyle
dc.contributor.authorFarrell, Sinead L.
dc.contributor.authorKurtz, Nathan T.
dc.contributor.authorHansen, Renee Mie Fredensborg
dc.date.accessioned2023-10-02T09:11:21Z
dc.date.available2023-10-02T09:11:21Z
dc.date.created2023-04-03T14:13:16Z
dc.date.issued2023
dc.identifier.citationThe Cryosphere. 2023, 17 (3), 1411-1429.en_US
dc.identifier.issn1994-0416
dc.identifier.urihttps://hdl.handle.net/11250/3093401
dc.description.abstractInformation about sea ice surface topography and related deformation is crucial for studies of sea ice mass balance, sea ice modeling, and ship navigation through the ice pack. The Ice, Cloud, and land Elevation Satellite-2 (ICESat-2), part of the National Aeronautics and Space Administration (NASA) Earth Observing System, has been on orbit for over 4 years, sensing the sea ice surface topography with six laser beams capable of capturing individual features such as pressure ridges. To assess the capabilities and uncertainties of ICESat-2 products, coincident high-resolution measurements of sea ice surface topography are required. During the yearlong Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition in the Arctic Ocean, we successfully carried out a coincident underflight of ICESat-2 with a helicopter-based airborne laser scanner (ALS), achieving an overlap of more than 100 km. Despite the comparably short data set, the high-resolution centimeter-scale measurements of the ALS can be used to evaluate the performance of ICESat-2 products. Our goal is to investigate how the sea ice surface roughness and topography are represented in different ICESat-2 products as well as how sensitive ICESat-2 products are to leads and small cracks in the ice cover. Here, we compare the ALS measurements with ICESat-2's primary sea ice height product, ATL07, and the high-fidelity surface elevation product developed by the University of Maryland (UMD). By applying a ridge-detection algorithm, we find that 16 % (4 %) of the number of obstacles in the ALS data set are found using the strong (weak) center beam in ATL07. Significantly higher detection rates of 42 % (30 %) are achieved when using the UMD product. While only one lead is indicated in ATL07 for the underflight, the ALS reveals many small, narrow, and only partly open cracks that appear to be overlooked by ATL07.en_US
dc.language.isoengen_US
dc.publisherEuropean Geosciences Union, EGUen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleLinking scales of sea ice surface topography: evaluation of ICESat-2 measurements with coincident helicopter laser scanning during MOSAiCen_US
dc.title.alternativeLinking scales of sea ice surface topography: evaluation of ICESat-2 measurements with coincident helicopter laser scanning during MOSAiCen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber1411-1429en_US
dc.source.volume17en_US
dc.source.journalThe Cryosphereen_US
dc.source.issue3en_US
dc.identifier.doi10.5194/tc-17-1411-2023
dc.identifier.cristin2139257
dc.relation.projectFramsenteret: 2551323 (SUDARCO)en_US
dc.relation.projectNorges forskningsråd: 325241en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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