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dc.contributor.authorVallot, Dorothee
dc.contributor.authorAdinugroho, Sigit
dc.contributor.authorStrand, Robin
dc.contributor.authorHow, Penelope
dc.contributor.authorPettersson, Rickard
dc.contributor.authorBenn, Douglas
dc.contributor.authorHulton, Nicholas R. J.
dc.date.accessioned2019-04-10T15:30:03Z
dc.date.available2019-04-10T15:30:03Z
dc.date.issued2019-03-29
dc.identifier258549414
dc.identifier8c6ac737-5a72-4e2f-a059-a7bdfd356fed
dc.identifier000462819000001
dc.identifier85065669220
dc.identifier000462819000001
dc.identifier.citationVallot , D , Adinugroho , S , Strand , R , How , P , Pettersson , R , Benn , D & Hulton , N R J 2019 , ' Automatic detection of calving events from time-lapse imagery at Tunabreen, Svalbard ' , Geoscientific Instrumentation Methods and Data Systems , vol. 8 , no. 1 , pp. 113-127 . https://doi.org/10.5194/gi-8-113-2019en
dc.identifier.issn2193-0856
dc.identifier.otherORCID: /0000-0002-3604-0886/work/64697377
dc.identifier.urihttps://hdl.handle.net/10023/17496
dc.description.abstractCalving is an important process in glacier systems terminating in the ocean, and more observations are needed to improve our understanding of the undergoing processes and parameterize calving in larger-scale models. Time-lapse cameras are good tools for monitoring calving fronts of glaciers and they have been used widely where conditions are favourable. However, automatic image analysis to detect and calculate the size of calving events has not been developed so far. Here, we present a method that fills this gap using image analysis tools. First, the calving front is segmented. Second, changes between two images are detected and a mask is produced to delimit the calving event. Third, we calculate the area given the front and camera positions as well as camera characteristics. To illustrate our method, we analyse two image time series from two cameras placed at different locations in 2014 and 2015 and compare the automatic detection results to a manual detection. We find a good match when the weather is favourable, but the method fails with dense fog or high illumination conditions. Furthermore, results show that calving events are more likely to occur (i) close to where subglacial meltwater plumes have been observed to rise at the front and (ii) close to one another.
dc.format.extent15
dc.format.extent5590935
dc.language.isoeng
dc.relation.ispartofGeoscientific Instrumentation Methods and Data Systemsen
dc.subjectGE Environmental Sciencesen
dc.subjectQA75 Electronic computers. Computer scienceen
dc.subjectNDASen
dc.subject.lccGEen
dc.subject.lccQA75en
dc.titleAutomatic detection of calving events from time-lapse imagery at Tunabreen, Svalbarden
dc.typeJournal articleen
dc.contributor.institutionUniversity of St Andrews. School of Geography & Sustainable Developmenten
dc.contributor.institutionUniversity of St Andrews. Bell-Edwards Geographic Data Instituteen
dc.identifier.doi10.5194/gi-8-113-2019
dc.description.statusPeer revieweden


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