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dc.contributor.authorThakuri, Sudeep
dc.contributor.authorSalerno, Franco
dc.contributor.authorBolch, Tobias
dc.contributor.authorGuyennon, Nicolas
dc.contributor.authorTartari, Gianni
dc.date.accessioned2019-03-13T15:30:12Z
dc.date.available2019-03-13T15:30:12Z
dc.date.issued2016-03
dc.identifier.citationThakuri , S , Salerno , F , Bolch , T , Guyennon , N & Tartari , G 2016 , ' Factors controlling the accelerated expansion of Imja Lake, Mount Everest region, Nepal ' , Annals of Glaciology , vol. 57 , no. 71 , pp. 245-257 . https://doi.org/10.3189/2016AoG71A063en
dc.identifier.issn0260-3055
dc.identifier.otherPURE: 258136802
dc.identifier.otherPURE UUID: 56d57b96-357c-4a41-801c-5e5ec4f22c91
dc.identifier.otherScopus: 84964374750
dc.identifier.otherORCID: /0000-0002-8201-5059/work/55379133
dc.identifier.urihttp://hdl.handle.net/10023/17281
dc.description.abstractThis study explores the link between area increase of Imja Tsho (Lake) and changes of Imja Glacier (area ∼25km2) under the influence of climate change using multitemporal satellite imagery and local climate data. Between 1962 and 2013, Imja Lake expanded from 0.03±0.01 to 1.35±0.05 km2 at a rate of 0.026±0.001 km2 a-1. The mean glacier-wide flow velocity was 37±30ma-1 during 1992-93 and 23±15ma-1 during 2013-14, indicating a decreasing velocity. A mean elevation change of -1.29±0.71ma-1 was observed over the lower part of the glacier in the period 2001-14, with a rate of -1.06±0.63ma-1 in 2001-08 and -1.56±0.80ma-1 in 2008-14. We conclude that the decrease in flow velocity is mainly associated with reduced accumulation due to a decrease in precipitation during the last few decades. Furthermore, glacier ablation has increased due to increasing maximum temperatures during the post-monsoon months. Decreased glacier flow velocities and increased mass losses induce the formation and subsequent expansion of glacial lakes under favourable topographic conditions.
dc.format.extent13
dc.language.isoeng
dc.relation.ispartofAnnals of Glaciologyen
dc.rights© The Author(s) 2016. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.en
dc.subjectClimate changeen
dc.subjectGlacier flowen
dc.subjectGlacier hazardsen
dc.subjectMountain glaciersen
dc.subjectRemote sensingen
dc.subjectGE Environmental Sciencesen
dc.subjectEarth-Surface Processesen
dc.subject3rd-DASen
dc.subject.lccGEen
dc.titleFactors controlling the accelerated expansion of Imja Lake, Mount Everest region, Nepalen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
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/10.3189/2016AoG71A063
dc.description.statusPeer revieweden


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