Fay Campbell
Research interests
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InterestsSnow Hydrology, Glaciology, Dye tracer studies, Supraglacial snowpack, Haut Glacier d'Arolla, Meltwater runoff;, Preferential flow paths, Ice layers, Percolation, Snow permeability, Glacier
Research experience
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Oct 2002–
Jan 2007Research: The role of the supraglacial snowpack in mediating meltwater delivery to glacier systems
University of Glasgow · School of Geographical and Earth Sciences · University of GlasgowGlasgowGlaciology, Glacier Hydrology, Snow, Snowpack Hydrology, Glacier Dynamics, Haut Glacier d´Arolla
Education
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Oct 2002–
Jan 2007University of Glasgow
Glacier Hydrology · PhDUnited Kingdom · Glasgow -
Oct 1998–
May 2002University of Glasgow
Geography · BScUnited Kingdom · Glasgow
Other
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LanguagesEnglish, German, some French
Publications
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2.10Impact points
Role of the supraglacial snowpack in mediating meltwater delivery to the glacier system as inferred from dye tracer investigations
Hydrological Processes. 01/2006; 20:969–985.
The supraglacial snowpack plays an important role in mediating the delivery of meltwater produced at the snowpack surface to the rest of the glacier system, with potential implications for both proglacial hydrograph form and the timing and magnitude of glacier movement induced by changes in subglaci... [more] The supraglacial snowpack plays an important role in mediating the delivery of meltwater produced at the snowpack surface to the rest of the glacier system, with potential implications for both proglacial hydrograph form and the timing and magnitude of glacier movement induced by changes in subglacial water pressure. However, there remain few field observations of the hydrological behaviour of supraglacial snowpacks and its seasonal evolution during the melt season. Data collected during the 2004 melt season at Haut Glacier d'Arolla, Valais, Switzerland, uses both qualitative and quantitative dye tracing techniques to enhance our understanding of supraglacial snowpack hydrology. Observations of the movement of dye-stained water show the complexity of flow patterns and the influence of ice layers and preferential flow zones in controlling percolation through the snowpack, and fluorometric techniques yield average flow rates for percolation through the snowpack of between 0·13 and 0·49 m h−1. The changing form of dye-return curves and increasing percolation rates reflect an increase over the course of the melt season in the efficiency with which the snowpack transmits meltwater. Snowpack permeability was found to be significantly lower (1·67 × 10−10 m2 on average) than that assumed in previous modelling studies of glacial hydrology, showing the need for improved information about snowpack hydrology if its importance in controlling runoff is to be fully appreciated.
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In the pink
Planet Earth. 01/2005;
Public interest article from the UK National Environment Research Council's magazine.
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The role of supraglacial snowpack hydrology in mediating meltwater delivery to glacier systems /
Ph.D. thesis submitted to the Department of Geographical and Earth Sciences, University of Glasgow, 2007. Thesis (Ph.D.) - University of Glasgow, 2007. Includes bibliographical references.... [more] Ph.D. thesis submitted to the Department of Geographical and Earth Sciences, University of Glasgow, 2007. Thesis (Ph.D.) - University of Glasgow, 2007. Includes bibliographical references.
Following (26)
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Stephanie Ann Greenstreet
The University of Nottingham -
Faye Stringer
Newcastle University -
Lalita Rose Balz
ResearchGate -
Christina Fiona Scherwionke
ResearchGate
4
Publications
39
Followers
Past advisors
University of Glasgow
University of Zurich
Prof. Trevor Hoey
University of Edinburgh
Dr Ross Purves
Prof. Pete Nienow