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dc.contributor.authorMölg, Nico
dc.contributor.authorFerguson, James
dc.contributor.authorBolch, Tobias
dc.contributor.authorVieli, Andreas
dc.date.accessioned2021-02-15T00:41:29Z
dc.date.available2021-02-15T00:41:29Z
dc.date.issued2020-02-15
dc.identifier.citationMölg , N , Ferguson , J , Bolch , T & Vieli , A 2020 , ' On the influence of debris cover on glacier morphology : how high-relief structures evolve from smooth surfaces ' , Geomorphology , vol. In press . https://doi.org/10.1016/j.geomorph.2020.107092en
dc.identifier.issn0169-555X
dc.identifier.otherPURE: 266448002
dc.identifier.otherPURE UUID: 34801ae5-22d7-4907-bf76-461dbde3b3a1
dc.identifier.otherRIS: urn:4B86373AA82FB6069E299D46383A1404
dc.identifier.otherORCID: /0000-0002-8201-5059/work/69463497
dc.identifier.otherScopus: 85080040137
dc.identifier.otherWOS: 000527306200005
dc.identifier.urihttp://hdl.handle.net/10023/21431
dc.descriptionThis study was funded by the SNSF project #200021_169775 “Understanding and quantifying the transient dynamics and evolution of debris-covered glaciers”.en
dc.description.abstractDebris-covered glaciers receive increasing attention during this period of sustained negative mass balance and expanding debris cover. The debris cover induces various feedback mechanisms that shape the evolution of the glacier geometry, and also of its surface. Although the surface morphology of many debris-covered glaciers is markedly different from that of debris-free glaciers, only a few studies have combined different processes to investigate these characteristic glacier surfaces in order to improve our knowledge of glacier evolution on a wider spatial and temporal scale. Debris-covered glacier tongues can consist of parts with a smooth surface as well as surfaces of high local relief with abundant ice cliffs in the lower end. In this study we analysed the evolution of the surface features of Zmuttgletscher, a debris-covered glacier in Switzerland, over a period of 140 years using time series of historic maps, high resolution digital elevation models and glacier velocities, as well as data on debris cover extent and thickness. Our results revealed insights into the up-glacier expansion of the debris cover over time and the formation of medial moraines in the prolongation of the uppermost areas where debris emerged on the glacier surface. Moraine ridge prominence increased during periods of negative mass balance, and troughs developed in debris-free areas between ridges, persisting even after a continuous debris cover had developed. The changing surface morphology inhibits across-glacier meltwater flow, both supra- and subglacially. Accordingly, we found that large cryo-valleys with ice cliffs have formed down-glacier of the troughs where meltwater runoff accumulates. The meanders of these valleys have enlarged over time, especially by ice cliff backwasting at steep slopes, and most of the glacier width today is affected by such high-relief erosion features. We find that about 75% of all ice cliffs are located in this high-relief zone. The volume lost at these erosion features has increased by a factor of five since the 1980s, but is still negligible in comparison to the high glacier-wide thinning rates.
dc.language.isoeng
dc.relation.ispartofGeomorphologyen
dc.rightsCopyright © 2020 Published by Elsevier B.V. This work has been made available online in accordance with publisher policies or with permission. Permission for further reuse of this content should be sought from the publisher or the rights holder. This is the author created accepted manuscript following peer review and may differ slightly from the final published version. The final published version of this work is available at https://doi.org/10.1016/j.geomorph.2020.107092en
dc.subjectDebris-covered glacieren
dc.subjectSurface morphologyen
dc.subjectIce cliffsen
dc.subjectMedial moraineen
dc.subjectG Geography (General)en
dc.subjectDASen
dc.subject.lccG1en
dc.titleOn the influence of debris cover on glacier morphology : how high-relief structures evolve from smooth surfacesen
dc.typeJournal articleen
dc.description.versionPostprinten
dc.contributor.institutionUniversity of St Andrews.School of Geography & Sustainable Developmenten
dc.contributor.institutionUniversity of St Andrews.Bell-Edwards Geographic Data Instituteen
dc.identifier.doihttps://doi.org/10.1016/j.geomorph.2020.107092
dc.description.statusPeer revieweden
dc.date.embargoedUntil2021-02-15


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