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dc.contributor.authorL’Abée-Lund, Jan
dc.contributor.authorVøllestad, Leif
dc.contributor.authorBrittain, John Edward
dc.contributor.authorKvambekk, Ånund Sigurd
dc.contributor.authorSolvang, Tord
dc.coverage.spatialNorwayen_US
dc.date.accessioned2021-05-25T08:46:06Z
dc.date.available2021-05-25T08:46:06Z
dc.date.issued2021
dc.identifier.urihttps://hdl.handle.net/11250/2756198
dc.description.abstractObservations from 1890 to 2020 of ice phenology for 101 Norwegian lakes were used to detect variation in ice phenology. The average date of ice break-up occurred later in spring with increasing elevation, latitude and longitude. The average date of freeze-up and the length of the ice-free period decreased with elevation and longitude. Lakes were completely frozen later recently in autumn. There is a significant trend for earlier break-up, later freeze-up and completely frozen lakes after 1991.en_US
dc.language.isoengen_US
dc.publisherCopernicus Publicationsen_US
dc.titleGeographic variation and temporal trends in ice phenology in Norwegian lakes during the period 1890–2020en_US
dc.typeJournal articleen_US
dc.source.pagenumber2333-2356en_US
dc.source.volume15en_US
dc.source.journalThe Cryosphereen_US
dc.source.issue5en_US


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