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dc.contributor.authorMishra, Aditya
dc.contributor.authorNainwal, H. C.
dc.contributor.authorBolch, Tobias
dc.contributor.authorShah, Sunil Singh
dc.contributor.authorShankar, R.
dc.date.accessioned2023-01-05T15:30:07Z
dc.date.available2023-01-05T15:30:07Z
dc.date.issued2023-06-01
dc.identifier.citationMishra , A , Nainwal , H C , Bolch , T , Shah , S S & Shankar , R 2023 , ' Glacier inventory and glacier changes (1994–2020) in the Upper Alaknanda Basin, Central Himalaya ' , Journal of Glaciology , vol. 69 , no. 275 , pp. 591-606 . https://doi.org/10.1017/jog.2022.87en
dc.identifier.issn0022-1430
dc.identifier.otherPURE: 282630679
dc.identifier.otherPURE UUID: caab93c6-8950-40b6-bfd1-6489e1d40eed
dc.identifier.otherRIS: urn:E4AA5DA50809EDBFA32E67AD87D1CE5A
dc.identifier.otherORCID: /0000-0002-8201-5059/work/125303146
dc.identifier.otherScopus: 85160769957
dc.identifier.urihttps://hdl.handle.net/10023/26684
dc.descriptionFunding: The field work at Satopanth Glacier was supported by SERB & DST, New Delhi (Grant No. SB/DGH-101/2015 and DST/CCP/NHC/158/2018), IMSc, Chennai and SAC-ISRO funded projects. Parts of the work were conducted in the framework of the project ‘Understanding and quantifying the transient dynamics and evolution of debris-covered glaciers’ funded by the Swiss National Science Foundation (Grant No. 200021-169775).en
dc.description.abstractHimalayan glaciers have been shrinking and losing mass rapidly since 1970s with an enhanced rate after 2000. The shrinkage is, however, quite heterogeneous and it is important to document individual glacier characteristics and their changes at the basin scale. We present an updated glacier inventory of the Upper Alaknanda Basin (UAB), Central Himalaya for the year 2020 and report area, debris cover and length changes for the periods 1994–2006 and 2006–2020 based on remote-sensing data. We identified 198 glaciers, comprising an area of 354.6 ± 8.5 km2, and classified them according to their size and morphology. The glaciers of the basin lost 4.2 ± 2.9% (0.16 ± 0.11% a−1) of their frontal area (from 368.6 ± 9.2 to 353.0 ± 5.3 km2) from 1994 to 2020. The average retreat rate was higher in the period 2006–2020 (13.3 ± 1.8 m a−1) in comparison to 1994–2006 (9.3 ± 1.9 m a−1). However, the area change rate was similar for the two periods (0.14 ± 0.27% a−1 for 1994–2006 and 0.16 ± 0.19% a−1 for 2006–2020). The debris-covered area has increased by 13.4 ± 4.4% from 1994 to 2020. A comparison with previous studies in UAB indicates consistent area loss of ~0.15% a−1 since the 1960s.
dc.format.extent16
dc.language.isoeng
dc.relation.ispartofJournal of Glaciologyen
dc.rightsCopyright © The Author(s), 2022. Published by Cambridge University Press This is an Open Access article, distributed under the terms of the Creative Commons Attribution-NonCommercial-ShareAlike licence (http://creativecommons.org/licenses/by-nc-sa/4.0), which permits non-commercial re-use, distribution, and reproduction in any medium, provided the same Creative Commons licence is used to distribute the re-used or adapted article and the original article is properly cited. The written permission of Cambridge University Press must be obtained prior to any commercial use.en
dc.subjectCentral Himalayaen
dc.subjectClimate changeen
dc.subjectDebris-covered glaciersen
dc.subjectGlacier changesen
dc.subjectGlacier inventoryen
dc.subjectGE Environmental Sciencesen
dc.subjectNDASen
dc.subjectSDG 13 - Climate Actionen
dc.subjectMCCen
dc.subject.lccGEen
dc.titleGlacier inventory and glacier changes (1994–2020) in the Upper Alaknanda Basin, Central Himalayaen
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.contributor.institutionUniversity of St Andrews. Environmental Change Research Groupen
dc.identifier.doihttps://doi.org/10.1017/jog.2022.87
dc.description.statusPeer revieweden


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