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Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/36452
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dc.contributor.authorBevan, Suzanne Len_UK
dc.contributor.authorLuckman, Adrian Jen_UK
dc.contributor.authorBenn, Douglas Ien_UK
dc.contributor.authorAdusumilli, Susheelen_UK
dc.contributor.authorCrawford, Annaen_UK
dc.date.accessioned2024-11-08T01:03:24Z-
dc.date.available2024-11-08T01:03:24Z-
dc.date.issued2021-07-19en_UK
dc.identifier.urihttp://hdl.handle.net/1893/36452-
dc.description.abstractBetween 2014 and 2017, ocean melt eroded a large cavity beneath and along the western margin of the fast-flowing core of Thwaites Glacier. Here we show that from 2017 to the end of 2020 the cavity persisted but did not expand. This behaviour, of melt concentrated at the grounding line within confined sub-shelf cavities, fits with prior observations and modelling studies. We also show that acceleration and thinning of Thwaites Glacier grounded ice continued, with an increase in speed of 400 m a−1 and a thinning rate of at least 1.5 m a−1, between 2012 and 2020.en_UK
dc.language.isoenen_UK
dc.publisherCopernicus GmbHen_UK
dc.relationBevan SL, Luckman AJ, Benn DI, Adusumilli S & Crawford A (2021) Brief communication: Thwaites Glacier cavity evolution. <i>The Cryosphere</i>, 15 (7), pp. 3317-3328. https://doi.org/10.5194/tc-15-3317-2021en_UK
dc.rightsThis work is distributed under the Creative Commons Attribution 4.0 License.en_UK
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/en_UK
dc.subjectEarth-Surface Processesen_UK
dc.subjectWater Science and Technologyen_UK
dc.titleBrief communication: Thwaites Glacier cavity evolutionen_UK
dc.typeJournal Articleen_UK
dc.identifier.doi10.5194/tc-15-3317-2021en_UK
dc.citation.jtitleCryosphereen_UK
dc.citation.issn1994-0424en_UK
dc.citation.volume15en_UK
dc.citation.issue7en_UK
dc.citation.spage3317en_UK
dc.citation.epage3328en_UK
dc.citation.publicationstatusPublisheden_UK
dc.citation.peerreviewedRefereeden_UK
dc.type.statusVoR - Version of Recorden_UK
dc.contributor.funderNatural Environment Research Councilen_UK
dc.contributor.funderNatural Environment Research Councilen_UK
dc.author.emailanna.crawford@stir.ac.uken_UK
dc.citation.date19/07/2021en_UK
dc.contributor.affiliationSwansea Universityen_UK
dc.contributor.affiliationSwansea Universityen_UK
dc.contributor.affiliationUniversity of St Andrewsen_UK
dc.contributor.affiliationUniversity of California, San Diegoen_UK
dc.contributor.affiliationBiological and Environmental Sciencesen_UK
dc.identifier.isiWOS:000674944300001en_UK
dc.identifier.scopusid2-s2.0-8511114703en_UK
dc.identifier.wtid1998279en_UK
dc.contributor.orcid0000-0003-2649-2982en_UK
dc.contributor.orcid0000-0002-9618-5905en_UK
dc.date.accepted2021-06-08en_UK
dcterms.dateAccepted2021-06-08en_UK
dc.date.filedepositdate2024-11-07en_UK
rioxxterms.typeJournal Article/Reviewen_UK
rioxxterms.versionVoRen_UK
local.rioxx.authorBevan, Suzanne L|0000-0003-2649-2982en_UK
local.rioxx.authorLuckman, Adrian J|0000-0002-9618-5905en_UK
local.rioxx.authorBenn, Douglas I|en_UK
local.rioxx.authorAdusumilli, Susheel|en_UK
local.rioxx.authorCrawford, Anna|en_UK
local.rioxx.projectNE/S006605/1|Natural Environment Research Council|http://dx.doi.org/10.13039/501100000270en_UK
local.rioxx.projectNE/P011365/1|Natural Environment Research Council|http://dx.doi.org/10.13039/501100000270en_UK
local.rioxx.freetoreaddate2024-11-07en_UK
local.rioxx.licencehttp://creativecommons.org/licenses/by/4.0/|2024-11-07|en_UK
local.rioxx.filenametc-15-3317-2021.pdfen_UK
local.rioxx.filecount1en_UK
local.rioxx.source1994-0424en_UK
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