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dc.contributor.authorKuipers Munneke, P.
dc.contributor.authorMcGrath, D.
dc.contributor.authorMedley, B.
dc.contributor.authorLuckman, A.
dc.contributor.authorBevan, S.
dc.contributor.authorKulessa, B.
dc.contributor.authorJansen, D.
dc.contributor.authorBooth, A.
dc.contributor.authorSmeets, P.
dc.contributor.authorHubbard, B.
dc.contributor.authorAshmore, D.
dc.contributor.authorVan den Broeke, M.
dc.contributor.authorSevestre, H.
dc.contributor.authorSteffen, K.
dc.contributor.authorShepherd, A.
dc.contributor.authorGourmelen, N.
dc.date.accessioned2017-12-01T16:30:12Z
dc.date.available2017-12-01T16:30:12Z
dc.date.issued2017-11-01
dc.identifier.citationKuipers Munneke , P , McGrath , D , Medley , B , Luckman , A , Bevan , S , Kulessa , B , Jansen , D , Booth , A , Smeets , P , Hubbard , B , Ashmore , D , Van den Broeke , M , Sevestre , H , Steffen , K , Shepherd , A & Gourmelen , N 2017 , ' Observationally constrained surface mass balance of Larsen C ice shelf, Antarctica ' Cryosphere , vol 11 , no. 6 , pp. 2411-2426 . DOI: 10.5194/tc-11-2411-2017en
dc.identifier.issn1994-0416
dc.identifier.otherPURE: 251679230
dc.identifier.otherPURE UUID: baf04fa8-b7d7-48bd-8e4c-f4b5f75cce56
dc.identifier.otherBibtex: urn:c6cd0571f145f5e4820a722c4b44587f
dc.identifier.otherScopus: 85032812109
dc.identifier.urihttp://hdl.handle.net/10023/12225
dc.descriptionThis work is funded by the Netherland Polar Programme, Netherlands Earth System Science Centre (NESSC), NSF OPP research grant 0732946, NERC/GEF grants NE/L006707/1, NE/L005409/1, NE/E012914/1, GEF loans 863, 890, 1028.en
dc.description.abstractThe surface mass balance (SMB) of the Larsen C ice shelf (LCIS), Antarctica, is poorly constrained due to a dearth of in situ observations. Combining several geophysical techniques, we reconstruct spatial and temporal patterns of SMB over the LCIS. Continuous time series of snow height (2.5–6 years) at five locations allow for multi-year estimates of seasonal and annual SMB over the LCIS. There is high interannual variability in SMB as well as spatial variability: in the north, SMB is 0.40 ± 0.06 to 0.41 ± 0.04 m w.e. year−1, while farther south, SMB is up to 0.50 ± 0.05 m w.e. year−1. This difference between north and south is corroborated by winter snow accumulation derived from an airborne radar survey from 2009, which showed an average snow thickness of 0.34 m w.e. north of 66° S, and 0.40 m w.e. south of 68° S. Analysis of ground-penetrating radar from several field campaigns allows for a longer-term perspective of spatial variations in SMB: a particularly strong and coherent reflection horizon below 25–44 m of water-equivalent ice and firn is observed in radargrams collected across the shelf. We propose that this horizon was formed synchronously across the ice shelf. Combining snow height observations, ground and airborne radar, and SMB output from a regional climate model yields a gridded estimate of SMB over the LCIS. It confirms that SMB increases from north to south, overprinted by a gradient of increasing SMB to the west, modulated in the west by föhn-induced sublimation. Previous observations show a strong decrease in firn air content toward the west, which we attribute to spatial patterns of melt, refreezing, and densification rather than SMB.en
dc.format.extent16en
dc.language.isoeng
dc.relation.ispartofCryosphereen
dc.rights© Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License.en
dc.subjectG Geography (General)en
dc.subjectGE Environmental Sciencesen
dc.subject3rd-DASen
dc.subject.lccG1en
dc.subject.lccGEen
dc.titleObservationally constrained surface mass balance of Larsen C ice shelf, Antarcticaen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews. School of Geography & Sustainable Developmenten
dc.identifier.doihttps://doi.org/10.5194/tc-11-2411-2017
dc.description.statusPeer revieweden


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