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dc.contributor.authorCompton, Kathleen
dc.contributor.authorBennett, Richard A.
dc.contributor.authorHreinsdóttir, Sigrún
dc.date.accessioned2016-02-25T12:56:39Z
dc.date.available2016-02-25T12:56:39Z
dc.date.issued2015-02-06
dc.identifier.citationCompton K, Bennett RA, Hreinsdóttir S (2015) Climate-driven vertical acceleration of Icelandic crust measured by continuous GPS geodesy. Geophysical Research Letters 42: 743–750. Available: http://dx.doi.org/10.1002/2014GL062446.
dc.identifier.issn0094-8276
dc.identifier.doi10.1002/2014GL062446
dc.identifier.urihttp://hdl.handle.net/10754/597783
dc.description.abstract© 2015 The Authors. Earth's present-day response to enhanced glacial melting resulting from climate change can be measured using Global Positioning System (GPS) technology. We present data from 62 continuously operating GPS instruments in Iceland. Statistically significant upward velocity and accelerations are recorded at 27 GPS stations, predominantly located in the Central Highlands region of Iceland, where present-day thinning of the Iceland ice caps results in velocities of more than 30mm/yr and uplift accelerations of 1-2mm/yr$^{2}$. We use our acceleration estimates to back calculate to a time of zero velocity, which coincides with the initiation of ice loss in Iceland from ice mass balance calculations and Arctic warming trends. We show, through a simple inversion, a direct relationship between ice mass balance measurements and vertical position and show that accelerated unloading is required to reproduce uplift observations for a simple elastic layer over viscoelastic half-space model.
dc.description.sponsorshipData presented in Figure 1 are available in Table S1 in the supporting information. K.C. is funded by NSF Graduate Research Fellowship award DGE-1143953 and the P.E.O. Scholar Award. The Central Highlands Iceland GPS network was funded by the University of Arizona and grants from NSF (EAR-0711446 to the University of Arizona) and the Icelandic Center for Research RANNIS (60243011 to the Nordic Volcanological Center, University of Iceland). Installation and operation of additional sites used in this study were led by the Icelandic Meteorological Office (IMO), University of Iceland, Penn State, ETH, Landmælingar Íslands, Landsvirkjun, Université de Savoie, Bayerische Akademie der Wissenschaften, and KAUST. REYK and HOFN are International GNSS Service stations. UNAVCO and the IMO provided the technical support.
dc.publisherAmerican Geophysical Union (AGU)
dc.subjectclimate change
dc.subjectglacial isostatic adjustment
dc.subjectGPS geodesy
dc.subjectIceland
dc.subjectuplift
dc.titleClimate-driven vertical acceleration of Icelandic crust measured by continuous GPS geodesy
dc.typeArticle
dc.identifier.journalGeophysical Research Letters
dc.contributor.institutionDepartment of Geosciences; University of Arizona; Tucson Arizona USA
dc.contributor.institutionInstitute of Earth Sciences; University of Iceland; Reykjavik Iceland
dc.contributor.institutionNow at GNS Science; Avalon New Zealand
dc.date.published-online2015-02-06
dc.date.published-print2015-02-16


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