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dc.contributor.authorBreen, Catherine
dc.contributor.authorVuyovich, Carrie
dc.contributor.authorOdden, John
dc.contributor.authorHall, Dorothy
dc.contributor.authorPrugh, Laura
dc.coverage.spatialNorwayen_US
dc.date.accessioned2024-06-06T12:30:42Z
dc.date.available2024-06-06T12:30:42Z
dc.date.created2023-06-29T13:35:54Z
dc.date.issued2023
dc.identifier.citationRemote Sensing of Environment. 2023, 295 .en_US
dc.identifier.issn0034-4257
dc.identifier.urihttps://hdl.handle.net/11250/3132932
dc.description.abstractSnow covers a maximum of 47 million km2 of Earth’s northern hemisphere each winter and is an important component of the planet’s energy balance, hydrology cycles, and ecosystems. Monitoring regional and global snow cover has increased in urgency in recent years due to warming temperatures and declines in snow cover extent. Optical satellite instruments provide large-scale observations of snow cover, but cloud cover and dense forest canopy can reduce accuracy in mapping snow cover. Remote camera networks deployed for wildlife monitoring operate below cloud cover and in forests, representing a virtually untapped source of snow cover observations to supplement satellite observations. Using images from 1181 wildlife cameras deployed by the Norwegian Institute for Nature Research (NINA), we compared snow cover extracted from camera images to Moderate Resolution Imaging Spectroradiometer (MODIS) snow cover products during winter months of 2018–2020. Ordinal snow classifications (scale = 0–4) from cameras were closely related to normalized difference snow index (NDSI) values from the MODIS Terra Snow Cover Daily L3 Global 500 m (MOD10A1) Collection 6 product (R2 = 0.70). Tree canopy cover, the normalized difference vegetation index (NDVI), and image color mode influenced agreement between camera images and MOD10A1 NDSI values. For MOD10A1F, MOD10A1’s corresponding cloud-gap filled product, agreement with cloud-gap filled values decreased from 78.5% to 56.4% in the first three days of cloudy periods and stabilized thereafter. Using our camera data as validation, we derived a threshold to create daily binary maps of snow cover from the MOD10A1 product. The threshold corresponding to snow presence was an NDSI value of 40.50, which closely matched a previously defined global binary threshold of 40 using the MOD10A2 8-day product. These analyses demonstrate the utility of camera trap networks for validation of snow cover products from satellite remote sensing, as well as their potential to identify sources of inaccuracy. Validation Norway Remote cameras Gap-filling MODIS Snowen_US
dc.language.isoengen_US
dc.rightsAn error occurred on the license name.*
dc.rights.uriAn error occurred getting the license - uri.*
dc.subjectValidationen_US
dc.subjectNorwayen_US
dc.subjectRemote camerasen_US
dc.subjectGap-fillingen_US
dc.subjectMODISen_US
dc.subjectSnowen_US
dc.titleEvaluating MODIS snow products using an extensive wildlife camera networken_US
dc.title.alternativeEvaluating MODIS snow products using an extensive wildlife camera networken_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionacceptedVersionen_US
dc.subject.nsiVDP::Samfunnsgeografi: 290en_US
dc.subject.nsiVDP::Human geography: 290en_US
dc.subject.nsiVDP::Samfunnsgeografi: 290en_US
dc.subject.nsiVDP::Human geography: 290en_US
dc.source.pagenumber1136-1148en_US
dc.source.volume295en_US
dc.source.journalRemote Sensing of Environmenten_US
dc.identifier.doi10.1016/j.rse.2023.113648
dc.identifier.cristin2159472
dc.relation.projectNorges forskningsråd: 251112en_US
dc.relation.projectNorges forskningsråd: 281092en_US
dc.source.articlenumber113648en_US
cristin.ispublishedtrue
cristin.fulltextpostprint
cristin.qualitycode2


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