Show simple item record

dc.contributor.authorL’Abée-Lund, Jan Henning
dc.contributor.authorVøllestad, Leif Asbjørn
dc.contributor.authorBrittain, John Edward
dc.contributor.authorKvambekk, Ånund Sigurd
dc.contributor.authorSolvang, Tord
dc.coverage.spatialNorwayen_US
dc.date.accessioned2021-04-21T11:37:25Z
dc.date.available2021-04-21T11:37:25Z
dc.date.issued2020
dc.identifier.urihttps://hdl.handle.net/11250/2738876
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 altitude, latitude and longitude. The average date of freeze-up and the length of the ice-free period decreased with altitude and longitude. Lakes were completely frozen later recently later in autumn. A significant trend for earlier break-up, later freeze-up and completely frozen lakes after 1991.en_US
dc.language.isoengen_US
dc.titleGeographic variation and temporal trends in ice phenology in Norwegian lakes over a centuryen_US
dc.typeJournal articleen_US
dc.source.journalThe Cryosphereen_US


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record