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dc.contributor.authorKokhanovsky, Alexander
dc.contributor.authorLamare, Maxim
dc.contributor.authorDanne, Olaf
dc.contributor.authorBrockmann, Carsten
dc.contributor.authorDumont, Marie
dc.contributor.authorPicard, Ghislain
dc.contributor.authorArnaud, Laurent
dc.contributor.authorFavier, Vincent
dc.contributor.authorJourdain, Bruno
dc.contributor.authorLe Meur, Emmanuel
dc.contributor.authorDi Mauro, Biagio
dc.contributor.authorAoki, Teruo
dc.contributor.authorNiwano, Masashi
dc.contributor.authorRozanov, Vladimir
dc.contributor.authorKorkin, Sergey
dc.contributor.authorKipfstuhl, Sepp
dc.contributor.authorFreitag, Johannes
dc.contributor.authorHoerhold, Maria
dc.contributor.authorZuhr, Alexandra
dc.contributor.authorVladimirova, Diana
dc.contributor.authorFaber, Anne-Katrine
dc.contributor.authorSteen-Larsen, Hans Christian
dc.contributor.authorWahl, Sonja
dc.contributor.authorAndersen, Jonas K.
dc.contributor.authorVandecrux, Baptiste
dc.contributor.authorvan As, Dirk
dc.contributor.authorMankoff, Kenneth D.
dc.contributor.authorKern, Michael
dc.contributor.authorZege, Eleonora
dc.contributor.authorBox, Jason E.
dc.date.accessioned2021-05-02T19:27:59Z
dc.date.available2021-05-02T19:27:59Z
dc.date.created2020-03-03T12:39:34Z
dc.date.issued2019
dc.PublishedRemote Sensing. 2019, 11:2280 (19), 1-43.en_US
dc.identifier.issn2072-4292
dc.identifier.urihttps://hdl.handle.net/11250/2740684
dc.description.abstractThe Sentinel Application Platform (SNAP) architecture facilitates Earth Observation data processing. In this work, we present results from a new Snow Processor for SNAP. We also describe physical principles behind the developed snow property retrieval technique based on the analysis of Ocean and Land Colour Instrument (OLCI) onboard Sentinel-3A/B measurements over clean and polluted snow fields. Using OLCI spectral reflectance measurements in the range 400–1020 nm, we derived important snow properties such as spectral and broadband albedo, snow specific surface area, snow extent and grain size on a spatial grid of 300 m. The algorithm also incorporated cloud screening and atmospheric correction procedures over snow surfaces. We present validation results using ground measurements from Antarctica, the Greenland ice sheet and the French Alps. We find the spectral albedo retrieved with accuracy of better than 3% on average, making our retrievals sufficient for a variety of applications. Broadband albedo is retrieved with the average accuracy of about 5% over snow. Therefore, the uncertainties of satellite retrievals are close to experimental errors of ground measurements. The retrieved surface grain size shows good agreement with ground observations. Snow specific surface area observations are also consistent with our OLCI retrievals. We present snow albedo and grain size mapping over the inland ice sheet of Greenland for areas including dry snow, melted/melting snow and impurity rich bare ice. The algorithm can be applied to OLCI Sentinel-3 measurements providing an opportunity for creation of long-term snow property records essential for climate monitoring and data assimilation studies—especially in the Arctic region, where we face rapid environmental changes including reduction of snow/ice extent and, therefore, planetary albedo.en_US
dc.language.isoengen_US
dc.publisherMDPIen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleRetrieval of snow properties from the Sentinel-3 Ocean and Land Colour Instrumenten_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2019 by the Authors.en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.doi10.3390/rs11192280
dc.identifier.cristin1799244
dc.source.journalRemote Sensingen_US
dc.source.4011:2280en_US
dc.source.1419en_US
dc.source.pagenumber1-43en_US


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