<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-09-24T14:45:27Z</responseDate><request verb="GetRecord" identifier="oai:www.repository.cam.ac.uk:1810/279685" metadataPrefix="uketd_dc">https://api.repository.cam.ac.uk/server/oai/request</request><GetRecord><record><header><identifier>oai:www.repository.cam.ac.uk:1810/279685</identifier><datestamp>2021-04-21T18:25:06Z</datestamp><setSpec>com_1810_183634</setSpec><setSpec>com_1810_256064</setSpec><setSpec>col_1810_214795</setSpec></header><metadata><uketd_dc:uketddc xmlns:uketd_dc="http://naca.central.cranfield.ac.uk/ethos-oai/2.0/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dcterms="http://purl.org/dc/terms/" xmlns:uketdterms="http://naca.central.cranfield.ac.uk/ethos-oai/terms/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://naca.central.cranfield.ac.uk/ethos-oai/2.0/ http://naca.central.cranfield.ac.uk/ethos-oai/2.0/uketd_dc.xsd">
   <dc:title>The response of Hagafellsjökull Vestari glacier, Iceland, to future climate scenarios computed with a dynamic glacier flowline model coupled to a degree-day mass balance model</dc:title>
   <dc:identifier xsi:type="dcterms:DOI">10.17863/CAM.27054</dc:identifier>
   <dc:creator>Pickett, Mark</dc:creator>
   <uketdterms:advisor>Sutton-Long, Peter</uketdterms:advisor>
   <dcterms:abstract>A dynamic glacier flowline model is coupled to a degree-day mass balance model with the purpose of modelling the response of Hagafellsjökull vestari glacier to future climate change scenarios. The degree-day mass balance model is calibrated using mass balance measurements for the period 1997-2007. The temperature and precipitation input for the calibration is provided by a combination of ERA-40 reanalysis data and local weather station records. The calibrated model shows good agreement with the measured mass balances (r2 = 0.95, RMSE = 0.68 m w.e.).&#xd;
The flowline model is then calibrated against the 2007 surface profile extracted from a DEM constructed from LiDAR data. During calibration the model is run from 1997 to 2007 with the mass balance input provided by the calibrated degree-day model. A number of changes had to be made to the model in order to achieve a good fit with the reference profile. These included a parameterisation of the basal mechanisms of movement (i.e. sliding and deformation of the bed) which was forced by the calculation of water flux at the base; and the introduction of a uniform basal melt rate. The calibrated model calculates the 2007 ice surface profile with an RMSE of 4.41 m. The need to introduce a basal melt rate of 0.8 m yr-1 suggests the presence under the glacier of a significant source of geothermal energy.&#xd;
A range of climate scenarios are imposed on the finalised model to predict the glacier’s behaviour between 2007 and 2109. In the ‘worst-case’ scenario the glacier will lose almost 80% of the 2007 ice volume over the next century. If there is no future climate change relative to the 1978-2007 30-year averages for temperature and precipitation, by 2109 the glacier will lose 30% of the 2007 ice volume and the glacier front will retreat by just over 5 km from its 2007 position.</dcterms:abstract>
   <uketdterms:institution>University of Cambridge</uketdterms:institution>
   <dcterms:issued>2009-10-02</dcterms:issued>
   <dc:type>Thesis</dc:type>
   <uketdterms:qualificationlevel>Masters</uketdterms:qualificationlevel>
   <uketdterms:qualificationname>Master of Philosophy (MPhil)</uketdterms:qualificationname>
   <dc:language>en</dc:language>
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   <dcterms:license>https://apollo8-f-pro.lib.cam.ac.uk/bitstreams/bd5c92d4-c0ed-40f4-9047-32f2846644a4/download</dcterms:license>
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   <dc:rights>https://www.rioxx.net/licenses/all-rights-reserved/</dc:rights>
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