Show simple item record

dc.contributor.authorSeier, Gernot
dc.contributor.authorAbermann, Jakob
dc.contributor.authorAndreassen, Liss Marie
dc.contributor.authorCarrivick, Jonathan L.
dc.contributor.authorKielland, Pål Hage
dc.contributor.authorLöffler, Karina
dc.contributor.authorNesje, Atle
dc.contributor.authorRobson, Benjamin Aubrey
dc.contributor.authorRøthe, Torgeir Opeland
dc.contributor.authorScheiber, Thomas
dc.contributor.authorWinkler, Stefan
dc.contributor.authorYde, Jacob Clement
dc.date.accessioned2023-11-14T13:42:14Z
dc.date.available2023-11-14T13:42:14Z
dc.date.created2023-10-05T14:06:10Z
dc.date.issued2023
dc.identifier.issn1085-3278
dc.identifier.urihttps://hdl.handle.net/11250/3102519
dc.description.abstractThe Jostedalsbreen is the largest ice cap in Norway and mainland Europe. Rapid retreat of many of its outlet glaciers since the 2000s has led to the formation of several glacial lakes. Processes causing the formation and expansion of glacial lakes and their interaction with a glacier and terminal moraine have not been widely addressed yet. In this study, we investigate the degradation of the front of the southeast-facing outlet glacier Austerdalsbreen. Based on a variety of remotely sensed data (UAV-based and airborne orthophotos and DEMs, satellite images), we analyze the coincident glacial and proglacial changes of Austerdalsbreen and quantify the evolution of this transition zone during the last decades. In particular, we focus on the short-term evolution of the glacial lake since 2010, we examine the context of a glacier advance in the 1990s, and we report long-term changes by utilizing 1960s imagery. We discuss the evolution and conditions of Austerdalsbreen compared to other outlet glaciers of Jostedalsbreen. Overall, the glacier terminus has experienced a recession in the last decades. The 1990s terminus advance was more restricted than at other nearby outlet glaciers due to glacier surface debris cover, which is a critical factor for the glacier and lake evolution. However, in the most recent period, since 2012, a distinct expansion of a glacial lake is quantifiable. Since the rates of glacier surface lowering also considerably increased since approximately 2017 and the glacier retreated since the beginning of the 2000s with a clear maximum length decrease in 2015, we interpret the recently formed glacial lake as a contributory factor of glacial changes.en_US
dc.language.isoengen_US
dc.publisherWileyen_US
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/deed.no*
dc.titleGlacier thinning, recession and advance, and the associated evolution of a glacial lake between 1966 and 2021 at Austerdalsbreen, western Norwayen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2023 the authorsen_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.doi10.1002/ldr.4923
dc.identifier.cristin2182094
dc.source.journalLand Degradation and Developmenten_US
dc.identifier.citationLand Degradation and Development. 2023.en_US


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record

Attribution-NonCommercial-NoDerivatives 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivatives 4.0 Internasjonal