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dc.contributor.authorSevestre, H.
dc.contributor.authorBenn, Doug I
dc.date.accessioned2016-03-01T00:12:50Z
dc.date.available2016-03-01T00:12:50Z
dc.date.issued2015-09-01
dc.identifier.citationSevestre , H & Benn , D I 2015 , ' Climatic and geometric controls on the global distribution of surge-type glaciers : implications for a unifying model of surging ' , Journal of Glaciology , vol. 61 , no. 228 , pp. 646-662 . https://doi.org/10.3189/2015JoG14J136en
dc.identifier.issn0022-1430
dc.identifier.otherPURE: 228658811
dc.identifier.otherPURE UUID: 0697330f-8a70-414c-a531-8e1d742f4bca
dc.identifier.otherScopus: 84942423967
dc.identifier.otherORCID: /0000-0002-3604-0886/work/64697368
dc.identifier.otherWOS: 000363002200004
dc.identifier.urihttp://hdl.handle.net/10023/8342
dc.descriptionFinancial support was provided by the ConocoPhillips Lundin Northern Area Program project CRIOS.en
dc.description.abstractControls on the global distribution of surge-type glaciers hold the keys to a better understanding of surge mechanisms. We investigate correlations between the distribution of surge-type glaciers and climatic and glacier geometry variables, using a new global geodatabase of 2317 surge-type glaciers. The highest densities of surge-type glaciers occur within an optimal climatic envelope bounded by temperature and precipitation thresholds. Across all regions with both surge-type and normal glaciers, the former are larger, especially at the cold, dry end of the climatic spectrum. A species distribution model, Maxent, accurately predicts the major clusters of surge-type glaciers using a series of climatic and glacier geometry variables, but under-predicts clusters found outside the climatically optimal surge zone. We interpret the results in terms of a new enthalpy cycle model. Steady states require a balance between enthalpy gains generated by the balance flux and losses via heat conduction and meltwater discharge. This condition can be most easily satisfied in cold, dry environments (thin, low-flux glaciers, efficient conductive heat losses) and warm, humid environments (high meltwater discharges). Intermediate conditions correspond to the optimal surge zone, where neither heat conduction nor runoff can effectively discharge enthalpy gains, and dynamic cycling can result.
dc.language.isoeng
dc.relation.ispartofJournal of Glaciologyen
dc.rightsCopyright 2015 International Glaciological Society. This work is made available online in accordance with the publisher’s policies. This is the final published version of the work, which was originally published at http://dx.doi.org/10.3189/2015JoG14J136en
dc.subjectEnergy balanceen
dc.subjectGlacier surgesen
dc.subjectIce and climateen
dc.subjectGE Environmental Sciencesen
dc.subject3rd-NDASen
dc.subjectBDCen
dc.subjectR2Cen
dc.subject.lccGEen
dc.titleClimatic and geometric controls on the global distribution of surge-type glaciers : implications for a unifying model of surgingen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews.Bell-Edwards Geographic Data Instituteen
dc.contributor.institutionUniversity of St Andrews.School of Geography & Sustainable Developmenten
dc.contributor.institutionUniversity of St Andrews.Geography & Sustainable Developmenten
dc.identifier.doihttps://doi.org/10.3189/2015JoG14J136
dc.description.statusPeer revieweden
dc.date.embargoedUntil2016-03-01


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