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QUANTIFYING UNCERTAINTY IN USING MULTIPLE DATASETS TO DETERMINE SPATIOTEMPORAL ICE MASS LOSS OVER 101 YEARS AT KÅRSAGLACIÄREN, SUB
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2016 (English)In: Geografiska Annaler. Series A, Physical Geography, ISSN 0435-3676, E-ISSN 1468-0459, Vol. 98, no 1, 61-79 p.Article in journal (Refereed) 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

Place, publisher, year, edition, pages
2016. Vol. 98, no 1, 61-79 p.
Keyword [en]
mountain glacier, mass balance, glacier reconstruction, glacier geometry
National Category
Natural Sciences
Identifiers
URN: urn:nbn:se:polar:diva-3463DOI: 10.1111/geoa.12123OAI: oai:DiVA.org:polar-3463DiVA: diva2:1080538
Available from: 2017-03-10 Created: 2017-03-10 Last updated: 2017-11-29

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Publisher's full texthttp://dx.doi.org/10.1111/geoa.12123
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Geografiska Annaler. Series A, Physical Geography
Natural Sciences

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