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QUANTIFYING UNCERTAINTY IN USING MULTIPLE DATASETS TO DETERMINE SPATIOTEMPORAL ICE MASS LOSS OVER 101 YEARS AT KÅRSAGLACIÄREN, SUB
Ansvarlig organisasjon
2016 (engelsk)Inngår i: Geografiska Annaler. Series A, Physical Geography, ISSN 0435-3676, E-ISSN 1468-0459, Vol. 98, nr 1, s. 61-79Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

Glacier mass balance and mass balance gradient are fundamentally affected by changes in glacier 3D geometry. Few studies have quantified changing mountain glacier 3D geometry, not least because of a dearth of suitable spatiotemporally distributed topographical information. Additionally, there can be significant uncertainty in georeferencing of historical data and subsequent calculations of the difference between successive surveys. This study presents multiple 3D glacier reconstructions and the associated mass balance response of Kårsaglaciären, which is a 0.89 ± 0.01 km2 mountain glacier in sub

sted, utgiver, år, opplag, sider
2016. Vol. 98, nr 1, s. 61-79
Emneord [en]
mountain glacier, mass balance, glacier reconstruction, glacier geometry
HSV kategori
Identifikatorer
URN: urn:nbn:se:polar:diva-3463DOI: 10.1111/geoa.12123OAI: oai:DiVA.org:polar-3463DiVA, id: diva2:1080538
Tilgjengelig fra: 2017-03-10 Laget: 2017-03-10 Sist oppdatert: 2017-11-29

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Forlagets fullteksthttp://dx.doi.org/10.1111/geoa.12123
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Geografiska Annaler. Series A, Physical Geography

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