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Thematische Bibliographien / Fox Glacier / Dissertationen

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Dissertationen zum Thema „Fox Glacier“

Autor: Grafiati

Veröffentlicht am 4. Juni 2021

Zuletzt aktualisiert am 1. Februar 2022

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1

Hamré, Moa. "Förutsättningar för jökellopp vid Fox Glacier, Nya Zeeland." Thesis, Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK), 2011. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-71989.

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A great number of tourists visits each day the Fox Glacier in New Zealand and are subjected todangers such as jökulhlaups. This phenomena can occur suddenly and in a destructive way when abuilt up of water suddenly bursts and releases large amounts of water. This is well known to happen atthe near by Franz Josef Glacier which has similar settings to Fox Glacier, but sparse previous researchon the subject indicates different results of whether jökulhlaups are present or not by Fox Glacier. Thisthesis therefore aims to study the conditions for jökulhlaups at the glacier. This is done by remotese

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2

H, Purdie. "Intra-annual variations in abaltion and surface velocity on the lower Fox Glacier, South Westland, New Zealand." Thesis, University of Canterbury. Geography, 2005. http://hdl.handle.net/10092/10451.

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3

Hayes, D. G. "An Investigation of visitor behaviour in recreation and tourism settings: a case study of natural hazard management at the Glaciers, Westland National Park, New Zealand." Lincoln University, 2008. http://hdl.handle.net/10182/942.

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Visitor non-compliance with protective recommendations is a major problem faced by recreational managers within natural environments. Although many studies have been conducted on noncompliant visitor behaviour within natural resource areas, few attempts have been made to gain an understanding of the behaviour, or to understand the decision making process. This dissertation seeks to address this gap by exploring salient motivations behind noncompliant behaviour within a natural recreation setting. The study was conducted over the summer of 2007-2008 within the popular tourist attractions of

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4

Espiner, Stephen. "The phenomenon of risk and its management in natural resource recreation and tourism settings : a case study of Fox and Franz Josef Glaciers, Westland National Park, New Zealand." Lincoln University, 2001. http://hdl.handle.net/10182/638.

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The significance of risk is growing in many Western societies, a phenomenon linked to increasing individualism, personal choice, and outcome uncertainty in multiple spheres of life. Despite being healthier and more physically protected from harm than any previous society, a serious concern for safety and risk control is emerging as a defining characteristic of modern social life. Within the context of a risk-averse society, this thesis investigates the nature and relevance of risk in natural resource recreation and tourism settings. Millions of people every day visit national parks and other p

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Diaz, Melisa A. "Geochemistry of soils from the Shackleton Glacier region, Antarctica, and implications for glacial history, salt dynamics, and biogeography." The Ohio State University, 2020. http://rave.ohiolink.edu/etdc/view?acc_num=osu1595542667761355.

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6

Foster, Lesley A. "Utilisation of remote sensing for the study of debris-covered glaciers : development and testing of techniques on Miage Glacier, Italian Alps." Thesis, University of Dundee, 2010. https://discovery.dundee.ac.uk/en/studentTheses/06d96169-df3b-49f0-b26c-f8f1ccc58e8d.

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An increase in the number of debris-covered glaciers and expansion of debris cover across many glaciers has been documented in many of the world’s major glacierised mountain ranges over the last 100 years. Debris cover has a profound impact on glacier mass balance with thick layers insulating the underlying ice and dramatically reducing ablation, while thin or patchy cover accelerates ablation through albedo reduction. Few debris-covered glaciers have been studied in comparison with ‘clean’ glaciers and their response to climatic change is uncertain. Remote sensing, integrated with field data,

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7

Sagredo, Esteban A. "Glacier sensitivity along the Andes: implication for paleoclimatic reconstructions of the Little Ice Age." University of Cincinnati / OhioLINK, 2012. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1342103681.

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8

Fujita, Koji, and 耕史藤田. "Effect of dust event timing on glacier runoff: sensitivity analysis for a Tibetan glacier." Wiley, 2007. http://hdl.handle.net/2237/11362.

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9

La, Frenierre Jeff David. "Assessing the Hydrologic Implications of Glacier Recession and the Potential for Water Resources Vulnerability at Volcan Chimborazo, Ecuador." The Ohio State University, 2014. http://rave.ohiolink.edu/etdc/view?acc_num=osu1402593347.

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10

Davis, Andrew D. (Andrew Donaldson). "Multi-parameter estimation in glacier models with adjoint and algorithmic differentiation." Thesis, Massachusetts Institute of Technology, 2012. http://hdl.handle.net/1721.1/72868.

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Thesis (S.M.)--Massachusetts Institute of Technology, Computation for Design and Optimization Program, 2012.<br>Cataloged from PDF version of thesis.<br>Includes bibliographical references (p. 75-77).<br>The cryosphere is comprised of about 33 million km³ of ice, which corresponds to 70 meters of global mean sea level equivalent [30]. Simulating continental ice masses, such as the Antarctic or Greenland Ice Sheets, requires computational models capturing abrupt changes in ice sheet dynamics, which are still poorly understood. Input parameters, such as basal drag and topography, have large effe

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11

Jaña, Obregón Ricardo. "Digital elevation models and delineation of antarctic glaciers using stereo capabilities of ASTER satellite images steps on the way for a glacier monitoring on the Antarctic Peninsula /." [S.l. : s.n.], 2006. http://nbn-resolving.de/urn:nbn:de:bsz:25-opus-37837.

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12

Smith, Nita Jane. "An ASTER Digital Elevation Model (DEM) for the Darwin-Hatherton Glacial System, Antarctica." Thesis, University of Canterbury. Geography, 2007. http://hdl.handle.net/10092/1480.

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The Darwin-Hatherton glacial system is an outlet glacial system in the Transantarctic Mountains, Antarctica, which drains ice from the East Antarctic Ice Sheet into the Ross Ice Shelf. This research provides remotely sensed data that can be used in modeling research for the Darwin-Hatherton glacial system, which in turn can be used in mass balance research for the West Antarctic Ice Sheet. Two improved digital elevation models (DEM) are produced to cover the lower Darwin Glacier and to cover the upper Darwin and Hatherton Glaciers. The new improved DEMs are generated from Advanced Spaceborne

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13

Schoenenberger, Katherine R. "LITTLE ICE AGE CHRONOLOGY FOR CLASSEN AND GODLEY GLACIERS, MOUNT COOK NATIONAL PARK, NEW ZEALAND." University of Cincinnati / OhioLINK, 2001. http://rave.ohiolink.edu/etdc/view?acc_num=ucin990634749.

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14

Marshall, Gareth John. "The effectiveness of spaceborne synthetic aperture radar for glacier monitoring." Thesis, University of Cambridge, 1996. https://www.repository.cam.ac.uk/handle/1810/268042.

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This work examines the effectiveness of spaceborne synthetic aperture radar (SAR) for investigating seasonally variable glaciological parameters, in particular its ability to discriminate glacier surface facies in order to estimate glacier mass balance. A multitemporal C-band SAR dataset of Nordenskiold Land, Spitsbergen, acquired by the ERS-1 satellite, is used for the analysis, which focuses on mountain glaciers rather than ice sheets. Validating field measurements of ice and snowpack parameters were obtained contemporaneously with two SAR images, prior to and during the ablation season. A g

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15

Dierckx, Marie. "Marine ice rheology from deformation experiments of ice shelf samples using a pneumatic compression device: implications for ice shelf stability." Doctoral thesis, Universite Libre de Bruxelles, 2013. http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/209505.

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Antarctic ice shelves control the ice flux from the continent to the ocean. As such, they play a major role in the stability of the ice sheet and its potential contribution to sea level rise, especially in the context of global change. Below some of these ice shelves, marine ice can be found which is a product of the Deep Thermohaline Circulation. Due to its specific genetic process, marine ice has intrinsic physical (grain size, ice fabric, bubble content, ) and chemical (impurities, water stable isotopes) properties, that differ from those of 'meteoric ice' formed on the continent through sn

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16

Noll, Christian John. "A geological framework for temporal sedimentary dynamics." [College Station, Tex. : Texas A&M University, 2008. http://hdl.handle.net/1969.1/ETD-TAMU-2354.

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17

Rose, Kathryn Clare. "A wireless multi-sensor subglacial probe for investigating the deforming glacier bed." Thesis, University of Southampton, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.485440.

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The mechanisms that control glacier dynamics and fast ice stream flow are still poorly understood, largely due to the inaccessibility of the subglacial environment. One of the ways to improve on current investigations is to broaden the methods used to monitor the subglacial environment. An autonomous multi-sensor wireless probe was developed for use within an Environmental Sensor Network at Briksdalsbreen, Norway. Probes were deployed at the base of boreholes, measuring temperature, pressure, resistance (a proxy for conductivity), case strain, and tilt, six times a day. The probes used radio_c

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18

Sunnegårdh, Sandra, and Thea Svensson. "Touch Glaciem : The Touch Screen for Soft Ice Machines." Thesis, KTH, Maskinkonstruktion (Inst.), 2012. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-176628.

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The Chinese company Ocean Power manufactures and exports soft ice cream machines to companies worldwide. Their machines have high functionality and robust design that enables a low-cost manufacturing. All machines have a control panel where settings of the machine and the ice cream can be ranged. The control panel is at present designed in accordance with an old indigenous design tradition. With increasing international influence and contact, the need of functionality and design is changing. To stay competitive Ocean Power requests a change and an improvement of the control panel. The device n

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19

Javan-Mashmool, Mandana. "Theoretical and experimental investigations for measuring interfacial bonding strength between ice and substrate." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 2005. http://theses.uqac.ca.

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20

Khamis, Kieran. "Climate change and glacier retreat in the French Pyrénées : implications for Alpine river ecosystems." Thesis, University of Birmingham, 2014. http://etheses.bham.ac.uk//id/eprint/4927/.

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Climate change disproportionately threatens alpine river ecosystems due to the strong connections between cryosphere, hydrology and physicochemical habitat. Our general understanding of how these systems will respond to warming is, however, based on conceptual models derived from studies undertaken at relatively small spatial scales. This research utilizes: (i) field data collected from five glacierized river basins in the French Pyrénées; (ii) field based experimentation; and (iii) climate/hydrological modelling, to improve understanding of alpine river ecosystem change. Despite a linear, har

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21

Smart, Martin James. "Deglaciation dynamics of the Feegletscher Nord, Switzerland : implications for glacio-fluvial sediment transfer." Thesis, University of Hertfordshire, 2015. http://hdl.handle.net/2299/17094.

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Understanding of the processes of sediment transfer within, and from, glaciated catchments is of fundamental importance in order to establish rates of sediment transfer and resultant landscape evolution. Rates of glacio-fluvial sediment transfer are strongly controlled by glacier meltwater runoff and the availability of sediments for entrainment. However, it is becoming apparent that recently deglaciated forefields can modify the patterns of suspended sediment transfer. Glacier shrinkage exposes areas of unstable glacigenic sediments that can be subject to reworking and redistribution, and, as

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22

Rootes, Camilla M. "The nature and use of trimlines for analysing 3-dimensional glacier change in rugged terrain." Thesis, University of Sheffield, 2018. http://etheses.whiterose.ac.uk/22341/.

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23

Araujo-Cabarcas, Juan Carlos. "Numerical methods for glacial isostatic adjustment models." Thesis, Uppsala universitet, Institutionen för informationsteknologi, 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-193856.

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Nordic countries experience post-glacial rebound, a movement where geographical contours slowly change elevation with respect to the mean sea level. The glacial isostatic adjustment (GIA) model aims to explain the phenomena, which combined with seismic data allows geoscientists to reconstruct elastic coefficients and viscosities of the Earth's lithosphere and upper mantle. The use of standard commercial codes are not adequate for GIA simulations and result in significant errors in the displacement field. This negative outcome suggests the development of GIA codes that include advection of pre

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24

Trenbirth, Hazel Elizabeth. "Direct lichenometry in southern Norway : lichen growth rates, environmental controls and implications for lichenometric dating." Thesis, Swansea University, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.678291.

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25

Dux, Andrew Martin. "Distribution and population characteristics of lake trout in Lake McDonald, Glacier National Park implications for suppression /." Thesis, Connect to this title online, 2005. http://etd.lib.montana.edu/etd/2005/dux/DuxA1205.pdf.

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Thesis (M.S.)--Montana State University--Bozeman, 2005.<br>Title from PDF t.p. (viewed on Mar. 30, 2008). Chairperson, Graduate Committee: Christopher S. Guy. Includes bibliographical references (p. 67-76).

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26

Wood, Chris, and Dan Smith. "Dendroglaciological Evidence for a Neoglacial Advance of the Saskatchewan Glacier, Banff National Park, Canadian Rocky Mountains." Tree-Ring Society, 2004. http://hdl.handle.net/10150/262633.

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Seventeen glacially sheared stumps in growth position and abundant detrital wood fragments were exposed by stream avulsion at the terminus of the Saskatchewan Glacier in 1999. The stumps lay buried beneath the glacier and over 5 m of glacial sediment until historical recession and stream incision exposed the 225- to 262-year-old stand of subalpine fir, Englemann spruce and whitebark pine trees. Crossdating and construction of two radiocarbon-controlled floating tree-ring chronologies showed that all the subfossil stumps and boles exposed at this location were killed during a Neoglacial advance

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27

Fox, A. M. "A distributed, physically based snow melt and runoff model for alpine glaciers." Thesis, University of Cambridge, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.599154.

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This thesis describes the development, testing and use of a distributed, physically based model of snow melt and runoff for alpine glaciers. A distributed version of a one-dimensional energy and mass balance snowpack model, SNTHERM, is coupled to a two-dimensional saturated flow model, MODFLOW, and is used to simulate meltwater production, vertical and lateral routing, storage and runoff across the temperate Haut Glacier d’Arolla, Switzerland at the beginning of the 2000 melt season. SNTHERM was first modified to incorporate an albedo scheme parameterised for this glacier, and to stimulate mel

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Davis, Andrew D. (Andrew Donaldson). "Prediction under uncertainty : from models for marine-terminating glaciers to Bayesian computation." Thesis, Massachusetts Institute of Technology, 2018. https://hdl.handle.net/1721.1/121812.

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Thesis: Ph. D. in Computational Science and Engineering, Massachusetts Institute of Technology, Department of Aeronautics and Astronautics, 2018<br>Cataloged from PDF version of thesis.<br>Includes bibliographical references (pages 255-266).<br>The polar ice sheets have enormous potential impact on future global mean sea level rise. Recent observations suggest they are losing mass to the ocean at an accelerated rate. Skillful prediction of the ice sheets' future mass loss remains difficult, however; observations of key variables are insufficient and physical processes are poorly understood. Ev

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Petrenko, Vasilii Victorovich. "A study of carbon-14 of paleoatmospheric methane for the last glacial termination from ancient glacial ice." Diss., Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC campuses, 2008. http://wwwlib.umi.com/cr/ucsd/fullcit?p3291947.

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Thesis (Ph. D.)--University of California, San Diego, 2008.<br>Title from first page of PDF file (viewed March 18, 2008). Available via ProQuest Digital Dissertations. Vita. Includes bibliographical references.

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Hekkers, Michael Leslie. "Climatic and Spatial Variations of Mount Rainier's Glaciers for the Last 12,000 Years." PDXScholar, 2010. https://pdxscholar.library.pdx.edu/open_access_etds/4951.

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Regional paleoclimatic proxies and current local climate variables and were analyzed to reconstruct paleoglaciers in an effort to assess glacier change On Mount Rainier. Despite the dry and generally warm conditions (sea surface temperatures (SST) -0.15°C to +1.8°C relative to current temperatures), the previously documented McNeeley II advance (10,900 - 9,950 cal yr B.P.) was likely produced by air temperature fluctuations. The average SST record and the terrestrial climate proxies show cooling temperatures with continued dryness between McNeeley II and the Burroughs Mountain advance (3,442 -

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31

Degenhardt, John Jerome. "A model for the development of a lobate alpine rock glacier in southwest Colorado, USA implications for water on Mars /." Texas A&M University, 2002. http://hdl.handle.net/1969/320.

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32

Dhanasekaran, Deepananthan. "A Locally Adaptive Spatial Interpolation Technique for the Generation of High-Resolution DEMs." The Ohio State University, 2011. http://rave.ohiolink.edu/etdc/view?acc_num=osu1306112037.

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33

Sen, Gupta Avirup. "Improving the Physical Processes and Model Integration Functionality of an Energy Balance Model for Snow and Glacier Melt." DigitalCommons@USU, 2014. https://digitalcommons.usu.edu/etd/3875.

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The Hindu-Kush Himalayan region possesses a large resource of snow and ice, which acts as a freshwater reservoir for irrigation, domestic water consumption or hydroelectric power for billions of people in South Asia. Monitoring hydrologic resources in this region is challenging because of the difficulty of installing and maintaining a climate and hydrologic monitoring network, limited transportation and communication infrastructure and difficult access to glaciers. As a result of the high, rugged topographic relief, ground observations in the region are extremely sparse. Reanalysis data offer

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34

Maier, Monika E. "Clark's Nutcracker Seed Harvest Patterns in Glacier National Park and a Novel Method for Monitoring Whitebark Pine Cones." DigitalCommons@USU, 2012. https://digitalcommons.usu.edu/etd/1275.

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Clark's Nutcracker (Nucifraga columbiana) is the primary seed disperser of whitebark pine (Pinus albicaulis), which is in decline throughout its range. There is concern that a decline in whitebark pine will lead to a subsequent decline in local populations of Clark's Nutcracker. Because natural regeneration depends on the presence of Clark's Nutcracker, the process of harvesting whitebark pine seeds needs to be fully understood. In addition, resource managers need a cost-effective method for monitoring nutcracker occurrence in whitebark pine stands during the seed harvest season. I visited ele

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35

Zhou, Hao Bevis Michael. "Layered cartesian half-space models for earth's elastic response to contemporary surface loading phenomena." Columbus, Ohio : Ohio State University, 2008. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1204657482.

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36

Stroup, Justin Sirico. "Glacial Lake Ojibway, lacustrine stratigraphy and implications for drainage." Cincinnati, Ohio : University of Cincinnati, 2009. http://rave.ohiolink.edu/etdc/view.cgi?acc_num=ucin1243303456.

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Thesis (M.S.)--University of Cincinnati, 2009.<br>Advisor: Thomas V. Lowell. Title from electronic thesis title page (viewed Aug. 18, 2009). Includes abstract. Keywords: Lake Ojibway; lacustrine; 8,200 year event; lake cores; XRF chemistry; stratigraphy; Laurentide; Ice proximal; varves; drainage; Canada. Includes bibliographical references.

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Nicholson, Lindsey. "Modelling melt beneath supraglacial debris : implications for the climatic response of debris-covered glaciers." Thesis, University of St Andrews, 2005. http://hdl.handle.net/10023/10264.

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Understanding how debris-covered glaciers respond to climate is necessary in order to evaluate future water resources and glacier flood hazard potential, and to make sense of the glacier chronology in mountain regions, In order achieve this, it is necessary to improve the current understanding of how surface debris affects glacier ablation rate, and to develop methods by which the ablation of debris-covered glaciers can be predicted under various climatic scenarios. This thesis develops a numerical surface energy balance model that uses simple meteorological data to calculate melt beneath a de

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38

Williams, Stephen Vincent. "Visual arctic navigation: techniques for autonomous agents in glacial environments." Diss., Georgia Institute of Technology, 2011. http://hdl.handle.net/1853/41135.

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Arctic regions are thought to be more sensitive to climate change fluctuations, making weather data from these regions more valuable for climate modeling. Scientists have expressed an interest in deploying a robotic sensor network in these areas, minimizing the exposure of human researchers to the harsh environment, while allowing dense, targeted data collection to commence. For any such robotic system to be successful, a certain set of base navigational functionality must be developed. Further, these navigational algorithms must rely on the types of low-cost sensors that would be viable for u

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Loving, Jolene LaVal. "Physical mechanisms for climate variability during glacial and interglacial periods /." Diss., Digital Dissertations Database. Restricted to UC campuses, 2004. http://uclibs.org/PID/11984.

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40

Stutz, James Edward II. "Reconstruction of LGM and Post LGM Glacial Environment of McMurdo Sound: Implications for Ice Dynamics, Depositional Systems and Glacial Isostatic Adjustment." The Ohio State University, 2012. http://rave.ohiolink.edu/etdc/view?acc_num=osu1324595182.

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41

Favey, Etienne. "Investigation and improvement of airborne laser scanning technique for monitoring surface elevation changes of glaciers /." Zürich, 2000. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=14045.

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42

Chase, Geneva Erin. "Late-Glacial Climate as Inferred fom Chironomid Assemblages in Lake Sediments from Aroostook County, Northeastern Maine." Fogler Library, University of Maine, 2004. http://www.library.umaine.edu/theses/pdf/ChaseGE2004.pdf.

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43

Barrett, Brian Edward. "Ground penetrating radar techniques for quantifying water distribution in glacial ice." Thesis, University of Leeds, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.441173.

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44

Dix, Justin K. "The use of high resolution geophysics for the investigation of submerged palaeo-glaciomarine environments." Thesis, University of St Andrews, 1996. http://hdl.handle.net/10023/15271.

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A multi-disciplinary, high resolution, geophysical investigation of a Scottish Sea loch has facilitated both the reconstruction of a detailed late Quaternary para-stratigraphic model and the critical assessment of the acquisition and analytical methodologies most appropriate for the study of submerged palaeo-glaciomarine environments. Loch Ainort, situated on the eastern coast of the Isle of Skye, has been surveyed using a 192 kHz echosounder, a 400 kHz side scan sonar and a 3.5 kHz sub-bottom profiler. Lithological calibration was provided by the analysis of both in situ core data and extant

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45

Roesch, Mike J. "IDENTIFYING WILDLIFE CROSSING ZONES FOR THE PRIORITIZATION OF HIGHWAY MITIGATION MEASURES ALONG U.S. HIGHWAY 2: WEST GLACIER, MT TO MILEPOST 193." The University of Montana, 2010. http://etd.lib.umt.edu/theses/available/etd-06092010-100319/.

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Highways have been shown to fragment wildlife habitats and populations. In order to mitigate the effects that highways have on wildlife, it is important to assess where wildlife appear to be moving in close proximity to the highway. I surveyed for wildlife trails that approached either side of a ~64 km stretch U.S. Highway 2 (US-2) and monitored these trails with remote cameras. Ungulates, especially deer, were the most commonly photographed animals on trails. A limited number of photographs were also taken of coyote, black bear, snowshoe hare, wolf, and cougar. Camera images showed that wildl

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46

Guarino, Thomas. "Symphonic Poem (for Orchestra)." University of Akron / OhioLINK, 2015. http://rave.ohiolink.edu/etdc/view?acc_num=akron1429641512.

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47

Gessese, Alelign Fekade. "Algorithms for Bed Topography Reconstruction in Geophysical Flows." Thesis, University of Canterbury. Mechanical Engineering, 2013. http://hdl.handle.net/10092/8673.

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Bed topography identification in open channel and glacier flows is of paramount importance for the study of the respective flows. In the former, the knowledge of the channel bed topography is required for modelling the hydrodynamics of open channel flows, fluvial hydraulics, flood propagation, and river flow monitoring. Indeed, flow models based on the Shallow Water Approximation require prior information on the channel bed topography to accurately capture the flow features. While in the latter, usable bedrock topographic information is very important for glacier flow modellers to accurately p

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Wallin, Åsa. "Investigating methods for identifying paleo surge-type glaciers or highly dynamical ice flows in Trygghamn, west Spitsbergen." Thesis, Stockholms universitet, Institutionen för naturgeografi, 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-131801.

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Surge-type glaciers exhibit a cyclic behaviour with an ice mass increase in the reservoir area during the inactive, quiescent phase and a rapid transportation of ice during the active, surge phase. In order to interpret the effects of climate change correctly it is important to distinguish between advances of surge-type glaciers and those of ‘normal’ glaciers, caused by climatic fluctuations. This is particularly important for the Arctic, which is predicted to experience the highest increase in temperature on the planet. The dynamic and mechanism of surge-type

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Mountain, Keith Richard. "A clear sky net radiation model for the high elevation glacial environment /." The Ohio State University, 1990. http://rave.ohiolink.edu/etdc/view?acc_num=osu1487681148542966.

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50

Stokes, Christopher Richard. "The geomorphology of palaeo-ice streams : identification, characterisation and implications for ice stream functioning." Thesis, University of Sheffield, 2001. http://etheses.whiterose.ac.uk/14815/.

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Ice streams are the dominant drainage pathways of contemporary ice sheets and their location and behaviour are viewed as key controls on ice sheet stability. Identifying palaeo-ice streams is of paramount importance if we are to produce accurate reconstructions of former ice sheets and examine their critical role in the oceanclimate system. Many workers have invoked palaeo-ice streams from a variety of former ice sheets, despite a limited understanding of their glacial geomorphology. This thesis addresses the problem by predicting several diagnostic geomorphological criteria indicative of ice

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