About the Project
This project aims to quantify the magnitude, variability and controls on fluxes of carbon dioxide (CO2) and methane (CH4), in supraglacial debris covers. The key output will be a robust estimate of the role of debris-covered glaciers in regional and global cycling of these important greenhouse gases. The worldwide significance of carbon and methane cycling in subglacial environments is well established, however, the magnitude and variability of similar processes at the surface of debris-covered glaciers is unknown. In principle, supraglacial debris provide an ideal environment for high rates of microbial activity and chemical weathering: an abundance of fresh mechanically-weathered rock, an unlimited supply of water and high levels of energy provided by sun and atmosphere. Initial measurements over an alpine glacier using a gas analyser have identified very high CO2 drawdown rates. Debris-covered glaciers could therefore be important global sinks of carbon due to the extensive areas of debris-covered ice in the world’s mountain ranges. Data will be collected through fieldwork on debris-covered glaciers in the Italian Alps (Year 1) and Svalbard (Year 2), involving i) direct measurements of CO2 and CH4 fluxes using an eddy-covariance system and portable greenhouse gas analyser and ii) measurements and sampling of debris sediments for analysis. Follow-up laboratory work will determine the minerals, carbon content and microbial communities present in debris covers to determine the relative roles of chemical weathering and microbial activity in carbon gas cycling. Training will be provided in field and laboratory techniques, and there is potential for the student to develop new methods to simulate rock debris chemical weathering in a laboratory. Project supervision will be provided by staff at Northumbria University and the University Centre in Svalbard (UNIS), with the opportunity for the student to spend an extended period learning techniques and undertaking analysis at UNIS.
Eligibility and How to Apply:
Please note eligibility requirement:
• Academic excellence of the proposed student i.e. 2:1 (or equivalent GPA from non-UK universities [preference for 1st class honours]); or a Masters (preference for Merit or above); or APEL evidence of substantial practitioner achievement.
• Appropriate IELTS score, if required.
• Applicants cannot apply for this funding if currently engaged in Doctoral study at Northumbria or elsewhere.
For further details of how to apply, entry requirements and the application form, see:
https://www.northumbria.ac.uk/research/postgraduate-research-degrees/how-to-apply/
Please note: Applications that do not include a research proposal of approximately 1,000 words (not a copy of the advert), or that do not include the advert reference (e.g. RDF18/…) will not be considered.
Deadline for applications: 28 January 2018
Start Date: 1 October 2018
Northumbria University takes pride in, and values, the quality and diversity of our staff. We welcome applications from all members of the community. The University holds an Athena SWAN Bronze award in recognition of our commitment to improving employment practices for the advancement of gender equality and is a member of the Euraxess network, which delivers information and support to professional researchers.
References
1. Shaw TE, Brock BW, Ayala A, Rutter N and Pellicciotti F. 2017. Centreline and cross-glacier air temperature variability on an Alpine glacier: assessing temperature distribution methods and their influence on melt model calculations. Journal of Glaciology, doi: 10.1017/jog.2017.65
2. Bravo C, Loriaux T, Rivera A and Brock BW (2017) Assessing glacier contribution to streamflow at Universidad Glacier, central Andes of Chile. Hydrology and Earth System Sciences, 21, 3249-3266, doi:10.5194/hess-21-3249-3266.
3. Carenzo M, Pellicciotti F, Mabillard J, Reid T and Brock BW (2016) An enhanced temperature index model for debris covered glaciers accounting for thickness effect. Advances in Water Resources, 94, 457-469, doi: 10.1016/j.advwatres.2016.05.001.
4. Shaw TE, Brock BW, Fyffe CL, Pellicciotti F, Rutter N and Diotri F (2016) Air temperature distribution and energy-balance modelling of a debris-covered glacier. Journal of Glaciology, 62(231), 185-198, doi:10.1017//jog.2016.31.
5. Hodson A, Brock BW, Pearce D, Laybourn-Parry J and Tranter M (2015) Cryospheric ecosystems: a synthesis of snowpack and glacial research Environmental Research Letters, 10, 110201, doi:10.1088/1748-9326/10/11/110201 IF 4.134, JR 23/221 Environ. Sciences.
6. Schauwecker S, Rohrer M, Huggel C, Kulkarni A, Ramanathan A, Salzmann N, Stoffel M, Thayyen R and Brock BW (2015) Remotely sensed debris thickness mapping of Bara Shigri Glacier, Indian Himalaya. Journal of Glaciology, 61(228), 675-688, doi: 10.3189/2015JoG14J102.
7. Collier E, Nicholson LI, Brock BW, Maussion F, Essery R and Bush ABG (2014) Representing moisture fluxes and phase changes in glacier debris cover using a reservoir approach. The Cryosphere, 8, doi: 10.5194/tc-8-1429-2014.
8. Fyffe CL, Reid TD, Brock BW, Kirkbride MP, Diolaiuti G, Smiraglia C and Diotri F (2014) A distributed energy-balance melt model of an alpine debris-covered glacier. Journal of Glaciology, 60(221), 587-602, doi:10.3189/2014JoG13J148.
9. Reid T and Brock BW (2014) Assessing ice-cliff backwasting its contribution to total ablation of debris-covered Miage Glacier, Mont Blanc massif, Italy. Journal of Glaciology, 60(219), 3-13, doi: 10.3189/2014LoG13J045.