Ocean Sciences PhD/MPhil


Ffeithiau’r cwrs

  • Enw: Ocean Sciences
  • Cymhwyster: PhD/MPhil
  • Hyd: PhD: 3 years full-time; MPhil: 2 years full-time

Supervision is available for research across all discipline areas in the School of Ocean Sciences.

Research Areas

Ocean Sciences with specialisations in the following:

  • Shelf Sea and Coastal Processes
  • Biogeochemistry and Palaeoceanography
  • Marine Ecosystems: Conservation and Resource Management

Research Opportunities

Please read the guidance notes and select your topic from the directory of PhD research degrees opportunities. Topics are listed by academic School and are based on the research interests of academic staff.


Facilities include the research vessel (Prince Madog), aquaculture facilities and a full range of modern analytical equipment needed to study the biology, physics, geology and chemistry of oceans and seas.

Research degrees

MPhil and PhD are research degrees and are awarded after the examination of a candidate's thesis, produced following a period of research.

While most candidates pursue research degrees on a full-time basis, in certain circumstances it is possible to offer them on a part-time basis. You may register for these degrees at the beginning of any month. The usual period of registration for research degrees is:

  • Full-time: MPhil 2 years / PhD 3 years
  • Part-time: MPhil 3 years / PhD 5 years

It is possible for you to complete the MPhil after studying for only one year full-time or two years part-time. If you are a PhD candidate with a relevant Master's degree or at least two years' relevant experience, your period of registration could possibly be of only two years' duration full-time or three years part-time. This arrangement would have to be agreed by your Head of Department and Supervisor before your research is started. We expect PhD students to produce and submit a thesis for examination within four years of starting a three-year programme.

Rhoddir cynnwys y cwrs ar gyfer arweiniad yn unig a gall newid.

Cyfleoedd Prosiect Ymchwil

Please note the research project opportunities detailed here are NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

If you are a European or International student this research programme is one of those which allows you to develop a research project proposal as an initial and integral part of a Combined English / Study Skills and Research Course at the University before starting the PhD/MPhil degree.

European and International candidates who have already reached the required level of English can apply for entry onto the project of their choice by presenting a relevant research proposal when applying for admission.

Alternatively you may also consider developing your own research proposal based on the research specialisms within the school.

The opportunities which are currently available are outlined below.

A 1,000 year seawater temperature reconstruction for the South Icelandic Shelf using stable isotopes from mollusc shells

Supervisor: Dr Paul Butler

T: +44 (0) 1248 382853 / E: p.g.butler@bangor.ac.uk

Supervisor: Prof. James Scourse

T: +44 (0) 1248 382876 / E: j.scourse@bangor.ac.uk

Researchers at School of Ocean Sciences, Bangor University, have recently completed a seawater temperature reconstruction for the North Icelandic Shelf based on stable oxygen isotopes from the shell of the long-lived bivalve mollusc Arctica islandica. The shell material used for the analyses has been precisely dated because annual banding patterns in the shell can be cross dated using statistical techniques derived from tree-ring research. (This means that it is possible to assign precise calendar dates to fossil shells if their lifetimes overlap with those of live collected shells with a known date of death.

The site of the A. islandica population on the North Icelandic Shelf is oceanographically complex because two distinct water masses (Arctic Water and Atlantic Water) combine there, and the relative strength of these two water masses has been shown to have changed over the past 1,000 years (Wanamaker et al 2012, Nature Communications). The interaction of the two water masses (which have their own distinct isotopic signatures and distinct temperature characteristics) complicates the interpretation of the stable oxygen isotope record in the shells. To clarify the interpretation, we propose an equivalent isotope-based reconstruction for the South Icelandic Shelf, where Atlantic Water predominates. The studentship will involve (a) the construction of a 1,000 year chronology using annual growth increments in A. Islandica shells from the South Icelandic Shelf; (b) milling of samples from the shells for stable isotope analysis; (c) conversion of the stable oxygen isotope data to seawater temperatures using standard equations.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Anthropogenic impacts on coastal ecosystems: the synergistic effects of multiple stressors

Supervisor: Dr Stuart Jenkins

T: +44 (0) 1248 382896 / E: s.jenkins@bangor.ac.uk

Increasing pressure on coastal ecosystems from a range of anthropogenic impacts has led to increasing concern about changes at the individual, population and community levels, leading to significant negative changes in the functioning of ecosystems. Much research has addressed the role of particular stressors on community and ecosystem change. However there is increasing realisation that focusing observational and experimental work on single stressors may underestimate impacts; multiple stressors which affect coastal ecosystems may interact in non-intuitive ways. This project will use the intertidal rocky shore habitat as a model system to understand the interactive nature of multiple stressors on community structure and ecosystem functioning using a field experimental approach.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Biology and population dynamics of commercially exploited fishes

Supervisor: Prof. Chris Richardson

T: +44 (0) 1248 382855 / E: c.a.richardson@bangor.ac.uk

Supervisor: Dr Ian McCarthy

T: +44 (0) 1248 382862 / E: i.mccarthy@bangor.ac.uk

Marine capture fisheries play a crucial role in providing a high quality protein source to an increasing global population. The demand for seafood is increasing but the FAO has recognised that the room for expansion in capture fisheries is limited and that science-based species-specific management plans are required in order to ensure that fisheries can continue to be exploited sustainably in the long-term. Underpinning the development of any fisheries management model is a comprehensive understanding of the population dynamics and biology of the target species to derive measures of age/size structure, growth, mortality and maturity. Such information is still lacking for many exploited species in the fisheries of developing nations. This could be provided for one or more target species through a programme of PhD research. An example of such an approach was the work conducted in the School on Argyrops spinfer (Journal of Applied Ichthyology 25(2009):559-564; Acta Ichthyologica et Piscatoria 41(2011):55-62) in Omani coastal waters.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Climatic buffering by structural habitat formed by macro algae

Supervisor: Dr Andrew Davies

T: +44 (0) 1248 382842 / E: andrew.j.davies@bangor.ac.uk

Macro algae form extensive canopies in intertidal zones around the world. The structure that large species form are responsible for changing a variety of conditions such as reducing dessication for understory species, reducing drag and increasing sediment deposition. In this project, we will assess how macro algae can buffer surrounding areas from the effect of climatic extremes. For example, it is common to observe stands of macro algae freezing in winter, but the extent to which they buffer temperature in the sediments and understories in unknown. This project will marry together electronic engineering for the design of high resolution temperature sensors that can be deployed for long periods within macroalgal stands, taxonomy and ecology.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Context dependent effects of soft-sediment ecosystem engineers on biodiversity and ecosystem functioning

Supervisor: Dr Jan Hiddink

T: +44 (0) 1248 382864 / E: j.hiddink@bangor.ac.uk

Globally, bottom trawling is the main source of disturbance to the seabed. Bottom trawls kill a large fraction of the benthic invertebrates that live on the seabed. Benthic invertebrates in turn are very important for the biogeochemistry of the seabed, as they affect the cycling of nutrients. Particularly important are ecosystem engineers in marine sediments, such as lugworms and mud shrimps, which mix the sediment (= bioturbation) and pump water through the sediment (= bio-irrigation). Both enhance the penetration of oxygen into the seabed. This can result in enhanced levels of biodiversity and is therefore an example of facilitation, and can change the nutrient fluxes at the seabed. However, bioturbation can also have negative effects on other species living in the seabed as it disturbs and potentially buries them.

We are currently lacking an understanding of the importance of the effect bioengineers on biodiversity and biogeochemistry under different environmental conditions, relative to the natural and temporal variation. The effect of bioturbation and bio-irrigation on the biogeochemistry of the sediment is likely to depend on the ambient environmental conditions. In areas of high tidal currents over coarse, non-cohesive, sediments, sediments are likely to be oxygenated to a depth of several centimetres regardless of the presence of bioengineers, while oxygenation in areas of low tidal currents over muddy, cohesive, sediments is likely to depend on the presence of bioengineers. The aim of this project is to quantify the importance of soft-sediment ecosystem engineers on the biodiversity and biogeochemistry in muddy and sandy sediments.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Coral Reef Resilience and Marine Protected Areas

Supervisor: Dr John Turner

T: +44 (0) 1248 382881 / E: j.turner@bangor.ac.uk

The resilience of corals reefs to major perturbations such as global climate change events is affected by localised anthropogenic impact. Therefore, established and enforced Marine Protected Areas (MPAs) may help confer greater resilience on coral reefs. Studies investigating overall measures of reef health, including benthic biodiversity, reproduction, fish biomass in established MPAs around the world help in our understanding of resistance and recovery, provided that threats outside of the MPA are also assessed and regulated where necessary. Research focuses on making appropriate assessments to support management.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Determining the age of decapod crustaceans

Supervisor: Prof. Chris Richardson

T: +44 (0) 1248 382855 / E: c.a.richardson@bangor.ac.uk

T: +44 (0) 1248 382864/ E: j.hiddink@bangor.ac.uk

Decapod crustaceans (crabs, lobsters and shrimps) are commercially important throughout the world. Stock assessment of crustaceans can be difficult since any growth rings deposited in their calcified exoskeleton are lost periodically during moulting. Demographic information has traditionally relied upon the analysis of length frequency distributions and the identification of distinct size classes of individuals within the populations. Recent work has reported the detection of growth bands in calcified regions of the eyestalk and gastric mill in shrimps, crabs, and lobsters.

This project will investigate the periodicity of growth lines in the eyestalk and gastric mill of larval, juvenile and adult shore crabs Carcinus maenas and lobsters Homarus gammarus. Using various growth stages of these crustaceans held under different experimental laboratory conditions the role of temperature, moulting and food on growth line formation in the eyestalk and gastric mill will be determined. This PhD would suit a student interested in studying the demography of crustacean populations, larval rearing and experimental techniques.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Does fishing impact upon the provision of ecosystem services?

Supervisors: Prof. Michel Kaiser and Dr Jan Hiddink

T: +44 (0) 1248 383751/ E: michel.kaiser@bangor.ac.uk

Demersal fishing activities have a number of wider ecosystem level impacts on marine ecosystems. Direct contact with the seabed leads to changes in biomass, production and habitat structure. Thus it is likely that the provision of ecosystem services is also changed. Understanding how these changes impact upon fish production would inform better management such that it should be possible to trade off the changes incurred in ecosystem services with production and harvest of fish.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Ecological responses to global warming - the role of phenotypic plasticity in marine benthic invertebrates

Supervisor: Dr Luis Gimenez

T: +44 (0) 1248 382904 / E: l.gimenez@bangor.ac.uk

Supervisor: Dr Stuart Jenkins

T: +44 (0) 1248 382896 / E: s.jenkins@bangor.ac.uk

The objective of this project is to understand how temperatures interact with resource supply to determine patterns of body size. Body size is a central life history trait, as it affects survival and fecundity of individuals and ultimately population persistence. Body size is negatively correlated with temperature in a number of marine organisms and many marine organisms experience important amounts of resource limitation at least in some critical part of their lives. In principle, food limitation should increase mismatches between metabolic demands and energy supply and so exacerbate the effect of high temperatures on body size. However, in organisms with complex life cycles, the nature of resource limitation can vary through ontogeny due to variations in physiology and habitat use. For instance in sessile organisms such as intertidal barnacles, food availability may limit growth during both larval and juvenile/adult lives, but space becomes a key resource during the benthic life. Thus, such organisms are good models to evaluate ontogenetic changes in the influence of resource supply and temperature on body size. This project therefore evaluates changes in body size occurring through adaptive plastic mechanisms or as the consequence of physiological constraints. This project has relevance in the context of climate change as it explore physiological and developmental mechanisms leading to changes in body size distribution of organisms as a consequence of warming.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Factors which influence seasonally stratified Shelf Sea surface mixed layer depth.

Supervisor: Dr Tom Rippeth

T: +44 (0) 1248 382293/ E: t.p.rippeth@bangor.ac.uk

The surface of the ocean acts as a critical interface linking the atmosphere and the ocean, with sea surface values of temperature and pCO2 therefore key determinates of the direction and magnitude of heat and carbon fluxes between the atmosphere and the ocean. A key parameter which helps determine the sea surface temperature and pCO2 is the depth of the surface mixed layer of the shelf seas. This parameter is poorly predicted using the current generation of numerical models.

The aim of this project is to improve the predictive capacity of shelf sea numerical models by improving the parameterisation of the vertical mixing processes determining the surface mixed layer depth.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

From glacial deposits to giant sediment waves: reconstructing sedimentary processes in the Irish Sea Basin after the retreat of the last British-Irish Ice Sheet.

Supervisor: Dr Katrien Van Landeghem

T: +44 (0) 1248 388161 / E: k.v.landeghem@bangor.ac.uk

The Irish Sea was occupied by ice during the Last Glacial Maximum (LGM, 24 ka BP), leaving behind glacial sediments that have since been reworked by currents in the marine environment. The resulting complexity of the seabed is well preserved, with glacially carved trenches, ice-moulded drumlin fields, sand banks and unusually large sediment waves (reaching world-record-breaking heights of 36 m).

The PhD candidate will thus integrate marine geophysical (seismic and multibeam echosounder) and sediment granulometry with palaeo-hydrodynamic model outputs (generated by external third parties) to reconstruct the morphological and sedimentological history of the Irish Sea. The Irish Sea's glacial legacy has various sedimentological and hydrodynamical components, and the aim is to understand the role of these various components in the subsequent evolution of the post-glacial seafloor.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Fully funded PhD available at the School of Ocean Sciences, Bangor University

One of the following PhD topics in marine science will be funded through the Gaynor Cemlyn-Jones Trust. Funding of the project (start date October 2019) will cover student tuition fees, a stipend of £15009 per annum and approximately £2000 research expenses per annum over three years.

Please apply with CV and covering letter to the named principle supervisor of the project in which you are interested by Friday August 16th. We aim to interview in early September.

Only UK/EU candidates need apply.

Investigating shipwreck scour to aid future offshore engineering

Supervisors: Dr Peter Robins, Dr Michael Roberts, Dr Dei Huws,

Partners: Minesto Ltd., Innes McCartney (Bournemouth University), Hayley Roberts (Bangor School of Law).

Offshore engineering projects are rapidly increasing due in-part to the growing marine renewables sector where large arrays of windfarms and other structures are being installed in coastal regions globally. Scour around seabed structures is contingent on several complex interacting factors: structure size and shape, orientation relative to flow, water depth and tidal flow, wave climate, sediment type and geology. Over time, scour can undermine the structures themselves, with feedbacks within arrays and impacts to sediment supply to surrounding coastlines. Simulating these processes is crucial. However, scour modelling at ocean scale (tens-to-hundreds of kilometres) requires improved modelling techniques since typical computational fluid dynamics that resolve scales of metres are impractical due to computational effort.

The Welsh coast contains >1000 shipwrecks, mostly dating back to WWI and WWII. Bangor University have undertaken 400 multibeam bathymetric surveys at 300 Welsh shipwreck sites. This extensive dataset presents a unique opportunity to simulate the morphodynamic impact of seabed structures, where the pattern/rate of disturbance (scour, sediment deposition) is unquantified. Hence, this dataset provides critical ground-truthing for morphodynamic models for application to future coastal engineering.

The primary aim of this PhD is to characterise morphodynamic behaviour in real energetic ocean environments across Wales by developing a morphodynamic model to replicate the scour typologies, hence produce a practical tool for application to future offshore engineering initiatives. The multibeam datasets will be analysed in conjunction with model output and seabed/geological maps. Correctly identifying these mainly unknown wrecks using marine archives will help understand the subsequent morphological change, but is also of historical and cultural importance for Wales. Recent structures monitored regularly over the last 6 years will be selected for further detailed surveys during the PhD, where the student will design and undertake multibeam/sub-bottom surveys and sediment sampling.

A state-of-the-art 3D sediment-tide-wave model will be developed for these key sites, optimising grid configurations and model parameterisations for simulating scour and sediment transport. Simulations will run over decadal timescales using multibeam bathymetry for retro-validation. Outcomes will be appropriate ocean-scale modelling methodologies (and limitations) for simulating scour. Finally, the model will be applied to a site near Anglesey where >20 renewable energy structures will be installed. Simulations will help optimise array design to minimise scour and feedbacks to the surrounding environment.

This PhD will equip the student with exceptional analytical and computational skills, combing high-performance computing with rich datasets and fieldwork experience, with valuable applications to all aspects of oceanography.

For further details and to apply please contact Dr Peter Robins in the School of Ocean Sciences, Bangor University p.robins@bangor.ac.uk

The historical ecology of Welsh sharks, skates and rays

Supervisors Dr Adel Heenan, Prof Jan Geert Hiddink, (School of Ocean Sciences, Bangor University); Dr Freya St John (School of Natural Sciences, Bangor University)

Associated partners Joanna Barker (Marine and Freshwater Project Manager, Zoological Society of London; Ben Wray (Marine Ecologist, Evidence, Policy and Permitting Directorate, Natural Resources Wales); Ruth Thurstan (Exeter University Lecturer in Historical Ecology)

Once considered common throughout Europe, Wales is likely one of the few locations in northern Europe hosting a viable population of the Critically Endangered Angelshark Squatina squatina. A lack of long-term data has previously hampered the population assessment of many rare elasmobranchs and scientists are increasingly using neglected data sources (e.g. newspapers, diaries and fishing logbooks) to understand how endangered populations have changed over time. By combining historical ecology with fisher-produced local ecological knowledge (LEK), Hiddink et al. (in press) revealed a 70% reduction in Welsh Angelshark over ~50 years. Importantly, reasons for this decline are unknown. It is also unclear whether Angelsharks were always restricted to small localised pockets due to habitat requirements, and whether the current hotspots in Wales (Cardigan Bay: Heessen et al. 2016) represent reproductively viable populations. This project will fill these information gaps by using historical ecology, local ecological knowledge and fish-habitat modelling, to understand the population trends of the Welsh Angelshark and other elasmobranchs.

Specifically the project will ask: How does nearshore fishing effort over time and space relate to elasmobranch population trends? What are the habitat requirements of Angelsharks? What has allowed the Angelshark to persist in Wales while disappearing in the rest of NW Europe?

By tackling these overarching questions, the project aims to understand the drivers of the historical range change and population status of Welsh elasmobranch species. These outputs will be used to identify areas that are likely to be suitable for Angelsharks. This will result in management measure recommendations to ensure critical elasmobranch habitats are protected.

The candidate will have supervisory and project support from an interdisciplinary team at Bangor University, the University of Exeter and the project partners at Natural Resources Wales and Zoological Society of London. This project offers unique opportunities for research and training in fisheries conservation and management.

Applicants must have a minimum of a UK Honours Degree at 2:1 degree (or equivalent) in Marine Biology, Ecology, Environmental Science or Geography and a demonstrated excellence in written and oral communication skills. An MSc with distinction in a relevant field, experience of statistical analyses, fisheries and/or local ecological knowledge and of working in a multidisciplinary field of research are all desirable qualities.

For further information visit Angelshark Project: Wales https://Angelsharknetwork.com/wales/

For further details and to apply please contact Dr Adel Heenan (a.heenan@bangor.ac.uk)

Resilience of saltmarsh ‘Blue Carbon’ storing to environmental change

Supervisors: Dr Martin Skov, Dr Jennifer Shepperson (School of Ocean Sciences) and Prof. William Austin (Univ. St. Andrews).

Associated partners: Dr Jordi Pages (CEAB, Spain), Mr Angus Garbutt (CEH), Prof. Hilary Kennedy (Bangor, emeritus).

Coastal ecosystems, such as salt marshes, may undergo sudden shifts in area extent, which affect a multitude of coastal processes. The causes for changes are often unknown, and the worry is that they will increase into the future. Understanding the drivers and the consequence of shifts in area cover is profoundly important to predicting the effects of emergent climate change. This PhD will examine the effects of saltmarsh areal change to ‘blue carbon’ storing – a globally important service delivered by salt marshes. Management of ecosystems for carbon capture is a key component of current mitigation of the effects of climate change. Yet, we do not know the resilience of our carbon stores to environmental change. This PhD studentship will sample carbon stocks and use radio-isotope date from salt marshes with known patterns of change (eroding, expanding, unchanged) to explore the over-arching hypothesis, that carbon capturing by salt marshes is resilient to environmental change. You will investigate the proportions of saltmarsh carbon that derives from other systems (terrestrial, marine) to infer the importance of ecosystem connectivity to carbon storing. The PhD will finally examine the causes for saltmarsh areal change, to predict the resilience of marsh carbon stores to future environmental change.

We seek a dynamic and inquisitive student with a strong interests in ecosystem processes. You must have a 2.1 or 1st class (or equivalent) BSc in a relevant science discipline, an interest in ecology and, ideally but not essentially, biogeochemistry. Training or experience with numerate science is desirable.

You will join a friendly and interactive team of students, postdocs and staff investigating saltmarsh resilience, ecology and management, and be affiliated to the C-SIDE project (https://www.c-side.org/). Supervisors and training: Dr Martin Skov (Bangor) saltmarsh ecology, blue carbon sampling, resilience and statistical design/analysis. Dr Jennifer Shepperson (Bangor): remote sensing, GIS analysis and spatial statistics. Professor William Austin (St Andrews University): radio-isotope analysis and interpretation. Further support: Dr Jordi Pagès (CEAB, Spain. Carbon resilience), Angus Garbutt (Centre for Ecology and Hydrology. Management application).

For further details and to apply please contact Dr Martin Skov of the School of Ocean Sciences, Bangor University mwskov@bangor.ac.uk

The role of palaeowaves in shaping Welsh coastal waters since the Last Glacial Maximum

Supervisors Dr Simon Neill, Dr Margot Saher, Dr Sophie Ward (School of Ocean Sciences) and Prof. Katsuto Uehara (Kyushu University, Japan).

This is an innovative modelling proposal designed to investigate the role of wind waves on the evolution of northwest European shelf seas sediment dynamics since the Last Glacial Maximum (21,000 years before present), when global sea level was ~130 m lower than it is today. Throughout much of the present-day Irish Sea, sediment transport is dominated by tidal currents; however, wave-induced sediment transport can dominate in shallower waters. Through consideration of wave- and tidal-induced sediment transport, it will be possible to compare how their relative influence on sediment dynamics has changed over time. This project focuses on developing a comprehensive coupled wave-tide-sediment model for the northwest European shelf seas (for palaeo-time slices, last 21,000 years). Outputs from the model will be validated against observed evolution of seabed sediment grainsize from age-constrained marine sediment cores. Such a well-constrained model would be a powerful tool, including for predicting significant changes in hydrographic and habitat patters with time; for reconstructing patterns of accumulation of sediments (for marine aggregate extraction); for assisting archaeology and conservation; and for further refinement of observations of sea-levels.

You will be trained in a wide range of research techniques, including ocean modelling on supercomputers, as well as having an opportunity to conduct laboratory work. You shall make use of existing large scale model outputs of winds, tides and palaeobathymetries as input to your regional model. This PhD project is well funded, and includes costs for you to attend several international conferences to present and discuss your research with world-class scientists. By the end of this PhD, you will have developed into an excellent independent researcher with a deep understanding of the evolution of shelf sea environments and equipped with excellent research skills suitable to either further pursue a career in palaeo-environmental studies, or to move onto other exciting challenges in the marine environment.

Throughout the project the appointee will be given the opportunity to meet with diverse groups within the scientific community, and to travel to international conferences to disseminate results and progress the project. Applicants should hold a minimum of a UK Honours Degree at 2:1 level or equivalent in subjects such as Oceanography, Coastal Marine Science, Civil Engineering, Quantitative Methods/Statistics, or Environmental Science. Applicants who additionally have a Master’s degree, or relevant work experience, will be particularly competitive.

For further details and to apply please contact Dr Simon Neill in the School of Ocean Sciences, Bangor University (s.p.neill@bangor.ac.uk).

West Wales in the Silurian and its influence on the erosion of the present day coastal landscape

Supervisors: Dr Jaco Baas, Dr Suzanna Jackson, Dr Katrien van Landeghem, Dr Dei Huws, Guy Springett

Sponsor: TRG Leeds (Bill McCaffrey, Marco Patacci)


Wales’ location on a passive continental margin contrasts with the Silurian, 440 million years ago, when Wales was situated on an active plate boundary, similar to subduction zones in SE Asia today. This past landscape defines today’s geomorphology and daily life. Most of Silurian West Wales was below sea level and giant oceanic landslides formed deposits that are superbly preserved in present-day coastal cliffs. Novel technologies, i.e. drone photography and terrestrial laser scanning, now permit comprehensive studies of the geological history preserved in these cliffs, leading to: (a) better models for the spatio-temporal evolution of the basin the underwater landslides flowed through; and (b) coastal erosion hazard maps based on the spatial arrangement of Silurian rocks of contrasting hardness. Combining these cliff face studies with onshore and offshore geomorphological and geophysical studies will further aid palaeo-landscape reconstruction.


  • Integrate onshore and offshore sedimentological, geomorphological, and geophysical methods to reconstruct key sedimentary processes and palaeo-landscape evolution in the Silurian, a present-day landscape-defining period in Welsh environmental history.
  • Determine how the Silurian rocks shape present-day landscapes and coastal bathymetries in West Wales since the last ice age.
  • Determine the erosion hazard of coastal cliffs using the spatial distribution of Silurian rocks of contrasting hardness.

What will you do?

  • Sedimentary logging, drone photography, terrestrial laser scanning, and stratigraphic correlation to build improved models of 3D oceanic-landslide driven sedimentation patterns in Silurian Wales as analogue for other oceanic systems.
  • Marine bathymetric, terrestrial topographic and subsurface data collection, using seismic and geo-electric profiling, multibeam echosounding, and Lidar, to aid the palaeo-environmental reconstruction of the ocean the landslides flowed through, and to determine the role of the Silurian rocks in the landscape evolution since the last ice age.
  • Combine the above sedimentological and geomorphological data to produce coastal cliff erosion hazard maps.

What will you receive?

You will receive support and training from experts in earth and marine sciences. The School of Ocean Sciences at BU is internationally renowned for coastal and marine, geological, geographical, and environmental research, supported by its state-of-the-art marine infrastructure, including the 35-m long research vessel Prince Madog and a fleet of smaller boats.

For further details and to apply please contact Dr Jaco Baas in the School of Ocean Sciences, Bangor University j.baas@bangor.ac.uk

The origin and evolution of offshore sand banks

Supervisors: Dr Simon Neill, Dr Peter Robins, Dr Matt Lewis (Bangor University); Dr Neil Mitchell (Manchester University)

Project partner: Rob Langman (MarineSpace Ltd)

Offshore sand banks are a strategic source of sediment for the construction industry, and due to their role in wave refraction and breaking they are important for protecting coastal communities from the impact of storm waves. Recent multibeam surveys of these systems have the potential to provide an unprecedented level of understanding of sand bank dynamics. However, since these sand banks have evolved into their present configuration over thousands of years, it is not known whether their evolution is a response to relatively high frequency moderate sized events (e.g. spring tidal currents) or as a result of low frequency more extreme events (e.g. storms).

In this project, you will use high resolution multibeam datasets to set up state-of-the-art wave/tide/sediment models of two contrasting sand bank systems: one in a region which has a history of dredging, and another which has evolved solely as a response to natural processes.

The modelling system will be applied to time slices of bathymetry over the recent geological past to simulate how the sand banks have evolved over time, and whether there are key time slices in the past when sand banks have changed mode from wave to tidally dominated systems, or vice-versa. You will quantify the influence of recent dredging activities in relation to the natural variability of the system, and investigate possible future impacts of marine renewable energy extraction in relation to natural variability of the sand banks, and the impacts of sea-level rise to nearshore wave climate and coastal flooding.

You will gain extensive experience in spatial and time series analysis of large complex in situ datasets, learn how to use such data to setup and parameterize numerical models, and gain extensive experience in running state-of-the-art coupled oceanographic models on supercomputers to examine the impacts of individual (storm) events, and evolution over seasonal and decadal time scales. This PhD will equip you with exceptional analytical and computational skills, combing high performance computing skills with rich complex multiple variable datasets to provide insight into temporal variability of shelf-sea dynamics, with applications to coastal flood risk, climate modelling methodologies, oceanography, marine renewable energy, fisheries, and sediment dynamics.

For further details and to apply please contact Dr Simon Neill in the School of Ocean Sciences, Bangor University s.p.neill@bangor.ac.uk

Shipwreck sites in Welsh waters as a proxy for ecosystem changes at renewable energy infrastructure sites.

Supervisors: Dr Katrien Van Landeghem: sediment dynamics, Dr Margot Saher: environmental reconstructions using foraminifera, Dr Martin Austin: flow/sediment dynamics, Dr Ronan Roche: benthic and pelagic communities, Dr Sophie Ward: coupling hydrodynamic and biogeochemical models.

Associated partners: CGG as funding industry project partner with David Gold, Mark Phips and Paul Tilyard, Dr David Assinder: marine biogeochemist, specialised in marine and estuarine pollution, Dr Michael Roberts: climate scientist, R&D manager

Scientific background: Artificial seabed objects impact the way the ecosystem functions, in turn directly impacting humans. A tool to predict these impacts would greatly assist in the environmental impact assessment for any seabed structure emplacement. Tighter coupling between sediment dynamics and benthic processes is needed to build such tool, and will be addressed via this PhD project.

Aim: Evaluating and predicting environmental impacts of artificial seabed structures. We will use shipwrecks as study objects as they are ubiquitous (representing different environments), well-documented (reducing the project risk), emplaced multiple decades ago (representing the life-span of typical seabed engineering projects) and part of The Crown Estate’s strategy to improve knowledge of our underwater cultural heritage.

What will you do?

1: Quantify the causal relationships between physical properties and ecological functions in the ecosystem around artificial seafloor objects.
-> Acquiring skills in marine geological, hydrodynamic, biological and biogeochemical sciences and in multivariate analysis of community data.

2: Validate a calibrated ecosystem model to better predict the long-term influence of the seafloor object on the surrounding site. -> Acquiring skills in ecosystem modelling and its programming language (FORTRAN).

3: Involve seabed infrastructure developers to ensure that extracting renewable tidal energy is designed with the knowledge of an environmental impact assessment, maximising positive effects and minimising adverse impacts.
-> Acquiring skills in hosting a workshop and collaborating with offshore engineers and environmental/heritage managers.

4: Help protect Wales’ underwater cultural heritage and educating people about their maritime heritage and its environmental impacts.

What will you receive? You will receive support and training from experts in marine sciences and extra research funding and support from industry sponsor CGG Robertson. The School of Ocean Sciences at BU is internationally renowned for coastal and shelf sea studies, supported by its state-of-the art marine infrastructure, including the 35m long Research Vessel Prince Madog and a fleet of smaller boats. You will receive specialist training in high resolution coupled ecosystem-hydrodynamic models. You will thus study truly integrated marine science and contribute towards a sustainable future of our coastal and marine environments.

For further details and to apply please contact Dr Katrien Van Landeghem in the School of Ocean Sciences, Bangor University k.v.landeghem@bangor.ac.uk

Coastal flooding: using historical records to predict and mitigate future risks

Supervisors: Dr Peter Robins, Dr Matt Lewis, Dr Martin Skov

Partners: National Library of Wales (NLW), Emmer Litt (NRW), Cai Ladd (Bangor/Swansea University), Ceris Jones (Aberystwyth University), Ivan Haigh (Southampton University).

Coastal flooding is ranked the second highest risk factor for civil emergency in the UK, responsible for at least £0.25bn annually in economic loss. Worse, in coming decades sea-level rise up to 1m is expected, together with wetter winters, which would drastically increase flood risk especially for towns situated on estuaries. Continued development of flood-prone areas, coastal engineering and catchment changes (e.g. deforestation, river dredging) will increase this threat further. The mitigation of future flood risk is therefore crucial for agencies responsible for UK estuaries. However, river flow predictions rarely capture the intensity and timings of flash floods in combination with other drivers such as storm surge and high tide. To achieve this requires new methodologies where the uncertainty associated with predictive inundation models is reduced and the interactions within the estuary are better understood.

Historical records of coastal flooding are essential for determining the probability of occurrence of hazards, as well as providing much-needed validation for inundation models. The National Library Wales archives has a unique and extensive dataset of well-documented coastal flooding events over the past two centuries (e.g. flood extent, depth, aerial photography, witness reports). This rich data presents an exceptional opportunity to study the complex interactions that lead to coastal flooding and address the following fundamental science questions: How do fluvial and marine processes and extremes vary across catchments and weather systems? How have estuaries changed with sea-level rise/coastal-engineering and what are the implications for flooding? Which estuary typologies are most vulnerable to flooding – is there a linear progression through estuary size or is there a tipping point where effects of flash floods are no longer felt? Will future climate and anthropogenic change alter flood risk and can we manage catchments to mitigate the risk?

This project will develop first-order perception of how coastal flood risks interact with environmental context, and how the risks will be moderated/exacerbated by sea-level rise, changing weather and land-use/geomorphic change, with practical emphasis on the Welsh coastline. During the course of the PhD, the student will develop modelling skills including validation methods, sensitivity of flood risk to boundary forcing and application to UKCP18 climate projections. They will curate a new flooding database for Wales and gain experience in time-series and spatial analysis techniques with GIS mapping application. The student will work with Natural Resources Wales to interact with shoreline management planning for coastal change and flood risks including sources-pathways-receptor methodology.

For further details and to apply please contact Dr Peter Robins in the School of Ocean Sciences, Bangor University p.robins@bangor.ac.uk

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Growth performance of aquatic animals under culture

Supervisor: Dr Ian McCarthy

T: +44 (0) 1248 382862 / E: i.mccarthy@bangor.ac.uk

Supervisor: Prof. Lewis Le Vay

T: +44 (0) 1248 388115 / E: l.levay@bangor.ac.uk

The demand for seafood as a high quality protein source is increasing with a growing global population. Seafood currently provides 3 billion people with 20% of their animal protein intake and per capita food fish intake is increasing. However, this demand cannot be met by increased capture fisheries production which has at around 90 million tonnes. It is clear that any future demand for seafood protein will be met through increased aquaculture production. Aquaculture production has risen in the last 3 decades (1980-2010) by almost 12 times, at an average annual rate of 8.8 per cent and currently stands at 64 million tonnes (2011) and is projected to overtake capture fisheries as the major source of food fish and a major contributor to food security. The School of Ocean Sciences has a long history of research into invertebrate and finfish aquaculture - both marine and freshwater, tropical and temperate, intensive and extensive production systems - and has expertise covering a wide range of research areas such as new species, developing/optimising culture techniques, diet development, feeding behaviour, growth performance, energetics, protein turnover, environmental impacts of aquaculture etc.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

How do waves interact with cohesive sea beds?

Supervisor: Dr Jaco Baas

T: +44 (0) 1248 382894 / E: j.baas@bangor.ac.uk

In the autumn of 2013, the international research project COHWAV investigated how waves interact with sea beds that contain mixtures of cohesive, “sticky” clay and cohesionless sand. Such beds are very common in nature, but surprisingly poorly studied and of fundamental importance for system-scale sediment transport modelling in the marine environment. This project was done on a near-field scale in a large wave facility at the University of Hull (“The Deep”). These laboratory experiments provided datasets that relate the properties of regular and irregular waves to the development of wave ripples on pure sand beds and on mixed sand- mud beds, using a state-of-art suite of instrumentation (e.g. acoustic bed profilers, ultrasonic velocity profilers, optical backscatter probes, and laser in-situ scattering and transmissometers). This PhD research project will have full access to the laboratory dataset with the aim to develop parameterisations that improve predictions of wave ripple growth and equilibrium size, as well as suspended sediment concentrations above these mixed-sediment bedforms. The PhD student will work within an international research group, in which scientists from universities in France (Caen/Rouen), the Netherlands (Utrecht) and the UK (Bangor, Hull, NOC Liverpool, Southampton) combine their expertise to increase the understanding of wave-substrate interaction in general and wave-generated bedforms in particular. The student will have the opportunity to lead similar experiments, but on a smaller scale, in the School of Ocean Sciences at Bangor University. These experiments could be extended by investigating flow-bed interaction in combined waves and tidal currents.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Hydrocarbon Reservoirs in Deep-Marine Sediments

Supervisor: Dr Jaco Baas

T: +44 (0) 1248 382894 / E: j.baas@bangor.ac.uk

Since the expansion of hydrocarbon exploration into the deep ocean (e.g. Gulf of Mexico, offshore West Africa, offshore Brazil) there has been an increased interest in the processes that transport sediment from terrestrial environments onto the continental margin, and in the architecture of large submarine fans in which this sediment is stored. Classical, simplistic models for the formation of turbidites and debris flow deposits have now been superseded by more realistic models that account for temporal and spatial variations in sediment gravity flow behaviour and for variations in the properties of sediment within these flows and within the underlying substrates (e.g. mixtures of cohesionless sand and cohesive mud). This is of fundamental importance in hydrocarbon reservoir analysis, because these models provide valuable information on the distribution of sand-prone and mud-prone lithofacies within deep-marine sedimentary sequences. In turn, this allows oil companies to make better predictions of the location of reservoir sands, source rocks, and baffles and barriers against the migration of hydrocarbons in sedimentary rocks.

This project combines laboratory studies and geological field studies to explore the dynamics and depositional products of sediment gravity flows that contain mixtures of cohesionless sand and cohesive clay. This is a research area that has seen rapid development and has prompted the interest of many oil companies, for example the companies that sponsor the work of the Turbidite Research Group (TRG Leeds), of which Dr Baas is an associate. Conceptual models of hybrid event beds (Haughton et al., 2009, Mar. Petrol. Geol.), transitional flow deposits (Baas et al. 2011, Sedimentology), and intrabed turbidites (Baas et al. 2014, Geology) will be tested in laboratory channels and in geological outcrops of deep-water basin sequences. This work builds upon several PhD and MSc projects in the past that have led to successful job applications in the hydrocarbon industry.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Individual variation in behavioural or physiological performance

Supervisor: Dr Ian McCarthy

T: +44 (0) 1248 382862 / E: i.mccarthy@bangor.ac.uk

Natural Selection operates on individuals but Science usually studies average responses. Although the value of understanding individual differences in performance was highlighted nearly 30 years ago by Bennett (1987), the common scientific approach has been to regard individual variation as 'noise' around some measurement of central tendency (e.g. mean, median) for the measured trait which is viewed as the more reliable / representative response. In fact, it is not uncommon to find that this average value does not actually exist within the group of individuals under study. In recent years the value of understanding the causes and consequence of inter-individual variation (IIV) in behavioural and physiological performance has been more widely recognised within the biological science community and is a growing area of research (e.g. Bell et al. 2009; Biro & Stamps, 2010; Réale et al., 2010; Careau & Garland, 2012). Consistent individual differences (CIDs) in physiology and behaviour drive individual fitness (i.e. survival and reproductive output) under variable environmental conditions and hence provide the framework through which natural selection can operate. Underlying this concept is the assumption that in order for selection to be able to operate, individuals will display repeatable levels of performance in fitness-related traits, i.e. they will maintain the same levels of performance and/or the same relative performance ranking over time compared to other individuals. This can result in selective mortality with surviving individuals exhibiting differential levels of performance in the pace of life continuum for that species in terms of growth, lifetime reproductive output and offspring quality.

The study of individual variation has been a central focus of my research activities since my PhD (1989-1992). This research has focussed on (1) describing individual variability in behavioural and physiological performance, e.g. differences in personality (aggression, feeding motivation), feeding behaviour, locomotor performance, metabolic rate and protein turnover, (2) quantifying repeatability/consistency of individual performance and (3) determining the ecological and life-history consequences of such variation. The aim of this project would be to develop a programme of research to investigate both intra-individual variation (i.e. repeatability/consistency of individual performance) and inter-individual variation (i.e. quantifying phenotypic variability within the population) for selected behavioural or physiological traits and to determine the life-history and fitness-related consequences of this observed variation.

References: Bennett (1987) New Directions in Ecological Physiology pp 147-169; Bell et al. (2009) Anim. Behav. 77, 771-783; Biro & Stamps (2010) Trends Ecol. Evol. 25, 653-659; Réale et al. (2010) Phil. Trans. R. Soc. 365, 4051-4063; Careau & Garland (2012) Physiol. Biochem. Zool. 85, 543-571.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Late Holocene sea-levels and high magnitude storm events in NW Wales

Supervisors: Prof. James Scourse, Dr Dei Huws, Prof. Geoff Duller (IGES, Aberystwyth University). External Supervisor: Dr Charles Bristow (Birkbeck College, London). Case Partner: Countryside Council for Wales (Dr Rod Jones)

T: +44 (0) 1248 382876 / E: j.scourse@bangor.ac.uk

T: +44 (0) 1248 382523 / E: d.g.huws@bangor.ac.uk

Different generations of geophysical models of the response of the Earth's surface to isostatic loading and unloading by ice and water predict rather different responses in terms of relative sea-level change for the late Holocene in NW Wales. The models by Lambeck (1995,1996, unpublished) predict that relative sea-levels in the region have been below Ordnance Datum (OD) throughout the entire deglaciation and Holocene, whereas those by Peltier (e.g. 1994) predict a late Holocene highstand of up to + 2.5 m OD around 4000 cal years BP, falling to the present. These differences result from the ice load and mantle rheology terms used in the different models. Calibration of these models with observational geological data is therefore necessary in order to improve model descriptions of both ice loading and mantle rheology. Significant advances have been made in the last three years in producing a refined relative sea-level curve for NW Wales deriving from radiocarbon dating of multiple sea-level index points preserved in thick sequences of interbedded peats and estuarine sediments cored in the NE Menai Strait (Roberts et al., in press). Sea-level index points have been corrected for temporal changes in tidal amplitude through palaeotidal modelling output (Uehara et al., 2006). However, no reliable sea-level index points exist for the period between 4000 cal. years BP and the present, precisely the interval within which the Peltier model predicts a highstand; additional sea-level data are therefore required for this period. Pilot study data exist relating to coastal morphosedimentary sequences in western Anglesey and the mainland adjacent to the SW entrance to the Menai Strait (Morfa Dinlle) which can be interpreted either in terms of a late Holocene highstand or high magnitude storm events, or both. Pocket beaches and coastal embayments at Llandwyn Island and elsewhere on the west Anglesey coast are characterised by moribund vegetated boulder clay cliffs and vegetated backshore testifying to either a highstand or extreme storm events in the recent Holocene. Similarly, at Morfa Dinlle a sequence of gravel beach ridges above OD might relate to a highstand, storm events, or both (Jones, 1999).

The aim of this CASE Studentship will be to test the alternative hypotheses 1. that there was a Holocene sea-level highstand in NW Wales (Peltier hypothesis) or 2. that the features can be explained in terms of erosion and deposition associated with extreme storm events without any highstand (Lambeck hypothesis). The data generated will also furnish evidence on the frequency of high magnitude storm events in NW Wales in the last few hundreds to thousands of years. The initial research phase will involve geomorphological mapping of the critical localities and survey by Leica 1200 GPS to define detailed elevations. This will be followed by geophysical survey to characterize sub-surface reflectors using ground penetrating radar (GPR). Sediment samples suitable for luminescence dating will be taken from open faces and in situ background radiation measured. The luminescence dates will constrain the chronology of the morphostratigraphic units. Given the time-consuming nature of luminescence dating, and the number of samples to be dated, we intend that in year 2 the student will undertake a significant component of the work in Aberystwyth; as such, this project falls within the Bangor –Aber Partnership and in particular the CCCR and C3W initiatives. Any materials suitable for radiocarbon dating will be measured via application to the NERC Radiocarbon Laboratory.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Optimal exploitation of multiple marine renewable energy resources

Supervisor: Dr Simon Neill

T: +44 (0) 1248 383938 / E: s.p.neill@bangor.ac.uk

To reduce greenhouse gas emissions and aid sustainable development, there is an urgent need to support our electricity generating capacity through the development of low carbon technologies, particularly those generated from renewable sources. The ocean represents a vast and largely untapped energy resource, which could be exploited as a form of low carbon electricity generation. However, marine renewable energy is intermittent, from the semi-diurnal and lunar nature of tidal currents, through to the seasonal and inter-annual nature of wave energy. Therefore, if marine energy is to provide firm power generation to the electricity network, it will be necessary to optimise its development by prioritising sites which are complementary in phase with one-another over a variety of timescales. In this project, you will develop a state-of-the-art coupled high resolution wave-tide model of the northwest European shelf seas – a world-leading marine energy resource – and apply swarm optimisation algorithms to the model outputs to generate optimal roadmaps of marine renewable energy for the UK and Europe beyond 2020. You will examine the sensitivity of the optimised roadmaps to different levels of marine energy and grid infrastructure investment, and determine how the roadmaps will vary for different scenarios of sea-level rise and future changes in weather patterns. By prioritising sites for marine renewable energy investment, results from this project will inform policy on how best to ensure cost-effective investment in the electricity grid, particularly as many of the key wave and tidal energy sites are remote from major demand in the southeast, and hence subject to significant transmission losses and potential blackouts.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Plankton phenology in response to inter-year variations in the timing of seasonal cycles of primary production

Supervisor: Dr Luis Gimenez

T: +44 (0) 1248 382904 / E: l.gimenez@bangor.ac.uk

Supervisor: Dr Stephanie Wilson

T: +44 (0) 1248 388141 / E: stephanie.wilson@bangor.ac.uk

In marine temperate systems primary production cycles seasonally and are usually characterised by a main peak in spring. Recruitment of many organisms depends on key life history stages matching these peaks of production. However, the timing, breadth and magnitude of these peaks may change from year to year leading to variations in the level of match/mismatch between organisms and its food. This project will examine the interrelationships between seasonal patterns of distribution of zooplankton (e.g. copepods, larval stages of benthic crustaceans), primary producers (e.g. diatoms) physical conditions of the water column and weather conditions. This work will be based on five years of weekly samples collected by the School of Ocean Sciences, at the Menai Straits as well as in subsequent collections done during the project.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Simulating tsunami generation, propagation and inundation using Smoothed Particle Hydrodynamics (SPH)

Supervisor: Dr Simon Neill

T: +44 (0) 1248 383938 / E: s.p.neill@bangor.ac.uk

Supervisor: Dr Reza Hashemi

T: +44 (0) 1248 383872 / E: r.hashemi@bangor.ac.uk

A recent study from a Japanese government-appointed team of scientists has estimated that 90 towns and cities in Japan must now consider how to withstand a tsunami impact higher than 10 m, and 23 of these have been advised to prepare for a tsunami which exceeds 20 m (Cyranoski, 2012). However, in terms of balancing risk against cost, it is important to know how water elevations will vary within these populated areas. Models of tsunami propagation and inundation are based on shallow-water equations formulated on Eulerian grids, with simplifications used to estimate overland flow. Such grid-based methods cannot simulate the complexity of multiple free-surfaces and the highly non-linear fluid dynamics of tsunamis which propagate far inland. For example, models of tsunami inundation cannot simulate two-phase fluid/sediment interaction, and such grid-based methods have difficulties in dealing with moving boundaries and sharp changes in topography (e.g. river channels and structures). With recent advances in high performance computing, one of the most exciting opportunities in the research field of fluid mechanics is the computationally expensive Lagrangian numerical method of Smoothed Particle Hydrodynamics (SPH). SPH was originally developed in the field of astrophysics, but its natural ability to capture large deformations and moving boundaries has led to its subsequent application to a wide range of fluid phenomena. In this project, SPH will be used to simulate tsunami generation, propagation and inundation, including coastal impact, overland bore propagation, two-phase fluid/sediment flow, and subsequent land drainage. This novel and exciting application of SPH to such a globally significant aspect of fluid dynamics has implications for risk reduction in tsunami hotspots.

Cyranoski (2012) Tsunami simulations scare Japan. Nature 484, 296-297.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

The future of vulnerable deep-sea ecosystems in a changing climate

Supervisor: Dr Andrew Davies

T: +44 (0) 1248 382842 / E: andrew.j.davies@bangor.ac.uk

Very little is known about organisms that are found in the deep sea. What is becoming clear is that they are under threat from climate change and anthropogenic impact, leading to calls for improved management of deep-sea habitats using tools such as networks of marine protected areas. However, at present, it is not possible to adopt such tools with any degree of confidence, because fundamental information on the distribution of many deep-sea organisms is lacking. Using state-of-the-art approaches, this studentship will develop comprehensive deep-sea climatology's that will be used to model suitable habitat for deep-sea ecosystem engineers. The proposed project represents an important step towards establishing the geographic distributions of these important organisms, predicting the influence of climate change on their distribution and determining how human impact extends over their habitat. This information will enhance our knowledge and facilitate effective international conservation and management of the deep sea.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

The Impact of seasonal Arctic Sea ice loss on air-sea fluxes of heat and momentum

Supervisor: Dr Tom Rippeth

T: +44 (0) 1248 382293/ E: t.p.rippeth@bangor.ac.uk

This PhD project proposes to address the question of how sea-ice and its absence affects the transfer of heat and momentum between the atmosphere and Arctic Ocean, with a particular emphasis on the dynamics of the Arctic Ocean polar mixed-layer. This question will be addressed using a combination of field observations and simple one-dimensional numerical modelling. The field observations were taken along the Eurasian sector of the Arctic Ocean and comprise hydrographic and microstructure turbulence data collected by the Bangor group and collaborators in recent years. The modelling component will utilise the General Ocean Turbulence Model (GOTM) turbulence closure model to simulate the vertical mixing and turbulent dissipation generated by boundary shear stresses under both ice and open water.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Tide-ocean circulation feedback in a warming climate

Supervisor: Dr Mattias Green

T: +44 (0) 1248 388161 / E: m.green@bangor.ac.uk

The climate controlling meridional overturning circulation (MOC) is sustained, if not controlled, by a continuous input of mechanical energy from wind (via eddies and direct upwelling) and tides (via abyssal internal waves). Since the generation of internal waves are dependent on both the tidal amplitudes and the vertical stratification there is a potential for future climate change to subtly modify the strength of the MOC by changing the tides, with potential feedback effects on the stratification itself.

Here we want to evaluate this potential feedback by the use of an existing climate model (OSUVic) and an established tidal model (OTIS) with an internal wave drag parameterisation to estimate the changes in abyssal mixing due to the changes in stratification in combination with future sea-level rise (SLR). Further experiments will look at extreme situations, e.g., impacts of halving or doubling the tidal amplitudes and extreme SLR and global warming, to obtain a probable range of future effects.


Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Understanding the transport of sand and mud in rivers and seas

Supervisor: Dr Jaco Baas

T: +44 (0) 1248 382894 / E: j.baas@bangor.ac.uk

Fine-grained cohesive sediment (clay, mud) is common in the natural environment, but it has not received as much attention as coarser-grained cohesionless sediment (sand, gravel). In fact, mixtures of sand and mud make up the vast majority of all sediment on Earth, but reliable models describing their dynamic behaviour in terms of erosion, transport and deposition are very rare. Such models are needed urgently to better predict the environmental impact of, for example, river floods, coastal floods, coastal erosion, siltation of harbours and navigation channels, and marine renewable energy schemes. The research project COHBED, in which 6 UK universities collaborate, has collected a large dataset on mixed cohesive sediment based on a unique combination of novel laboratory and field techniques. COHBED focuses on the development of sedimentary bedforms (dunes and ripples) in mixtures of sand and mud, but it also studies the biological processes that influence the movement of these sediments.

This PhD research project centres on the analysis of readily available, high-quality laboratory and field data, but there are also opportunities to collect new laboratory and field data. The student will benefit from the wide range of physical sedimentological and biological expertise within COHBED, including measurement techniques (e.g. Multibeam echo sounding, acoustic velocity profiling, acoustic suspended sediment concentration and size profiling, flock characterisation, and physical and biological sediment geotechnics). This project is well suited for students with a multidisciplinary interest that includes geophysics, sedimentology, microbiology and hydraulic engineering.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Zooplankton faecal pellet characteristics and contribution to elemental fluxes on the shelf seas

Supervisor: Dr Stephanie Wilson

T: +44 (0) 1248 388141 / E: stephanie.wilson@bangor.ac.uk

This project is part of the larger CArbon/Nutrient DYnamics and FLuxes Of the Shelf System (CANDYFLOSS) program. CANDYFLOSS will ask the question: How do shelf seas contribute to the global removal of CO2 from the atmosphere and the storage of carbon and nutrients in the ocean interior? The continental shelf regions of the ocean are highly productive and with only 5% of the global ocean area, support up to 20% of the world's primary production. This region therefore plays an important role in the global carbon cycle. Zooplankton also play an important role in the cycling of carbon and nutrients in the pelagic environment by feeding on phytoplankton and aggregates and packaging them into faecal pellets which can be recycled in the water column by bacteria and other plankton or exported to depth. Zooplankton themselves are also sources of nutrition for higher trophic levels such as fish, whales, and seabirds.

The aim of this project is to look at the role zooplankton play in the global carbon cycle on the continental shelf. The role of the student will be to participate in approximately 4 research cruises in the Celtic Sea during 2014 to observe and record zooplankton faecal pellets within sediment trap samples from a marine snow catcher device as well as collect live zooplankton for incubation and enumeration experiments. The student will then quantify the potential POC flux of the major zooplankton species and calculate the contribution zooplankton make to POC flux in this region using both microscopy and image analysing techniques.

Please note this research project opportunity is NOT funded by the University. Candidates must secure their own funding to meet the costs of PhD study.

Gofynion Mynediad

An upper second class honours degree (or equivalent from a non-UK institution) in natural science is required.

Sut i Ymgeisio

Cyngor ar wneud cais

Mae ceisiadau ar gyfer graddau ymchwil yn wahanol i geisiadau am gyrsiau ôl-radd trwy ddysgu fel gradd Feistr. Er bod y ffurflen gais yr un ffurflen, mae’r ffordd y dylech fynd ati i wneud cais yn gwneud gwahaniaeth.

Gwneud cais ar gyfer PhD/Mphil wedi ei ariannu’n allanol neu gennych chi eich hun

Fel gydag ein holl gyrsiau, gallwch ariannu cwrs PhD/Mphil ym Mangor eich hun, neu efallai fod gennych gymorth ariannol allanol (er enghraifft gan eich cyflogwr neu gan y cynulliad), ac rydym yn croesawu pob cais am wneud hynny. Er hynny, yn hytrach na chwblhau ffurflen gais yn unig, gallwch gymryd camau syml er mwyn gwneud yn siŵr fod eich cais yn sefyll allan ac yn fwy tebygol o fod yn llwyddiannus.

Mae pob myfyriwr PhD/Mphil angen goruchwyliaeth gan o leiaf un aelod o staff y Brifysgol, ac os ydych yn ystyried PhD/Mphil mae gennych eisoes syniad o’r pwnc neu’r maes yr ydym am astudio ynddo. I wneud yn siŵr fod gan y Brifysgol arbenigedd yn y maes er mwyn darparu goruchwyliaeth, edrychwch yn gyntaf ar ein tudalennau staff.

Unwaith yr ydych wedi dod o hyd i aelod o staff sydd yn gwneud gwaith ymchwil yn y maes, gallwch gysylltu â hwy yn uniongyrchol gyda chrynodeb o’ch ymchwil sy’n amlinellu eich cais a gofynnwch a ydynt yn fodlon i oruchwylio eich project. Os yw’r aelod o staff academaidd yn dangos diddordeb, gallwch drafod ymhellach i ddatblygu cynnig ymchwil PhD/Mphil llawn.

Ar yr adeg yma, dylech wneud cais am y rhaglen PhD/Mphil gan ddefnyddio'r ffurflen sydd ar gael yma. Dylech gwblhau’r ffurflen yn llawn gan gynnwys cyfeirnodau academaidd, eich cais ymchwil ac enw’r aelod o staff academaidd sydd am eich goruchwylio.

Ymgeisio am ysgoloriaethau PhD a hysbysebir gan Brifysgol Bangor

Eich cynnig ymchwil

Mae cynnig ymchwil da yn hanfodol os ydych yn ymgeisio am PhD neu MPhil. Dylai’r cynnig gynnwys:

(i) Trosolwg - rhowch fraslun o'r maes pwnc yr ydych am ymchwilio iddo, a rhoddwch wybodaeth am y dadleuon damcaniaethol, polisi ac empirig y byddwch yn ymdrin â hwy.
(ii) Cynllunio – rhaid i chi ddangos eich bod yn ymwybodol o amserlenni ymchwil, a bod gennych gynllun i reoli'ch gwaith. Rhaid i chi ddangos ei bod yn bosib cyflawni'r ymchwil yn yr amser sydd ar gael.
(iii) Cyfeiriadau llenyddol – rhaid i chi ddangos nad yw'ch maes ymchwil arfaethedig wedi'i astudio o'r blaen. Rhowch gyfeiriadau at erthyglau a thestunau llenyddol sy'n berthnasol i'ch maes astudio chi.
(iv) Methodoleg – rhaid i chi ddangos eich bod yn ymwybodol o'r offer methodolegol sydd ar gael, a nodi pa rai fyddai'n addas i'ch ymchwil chi.

Mwy o gyngor am baratoi eich cynnig ymchwil

Ymgeisio am ysgoloriaethau PhD a hysbysebir gan Brifysgol Bangor

Mae cyfleoedd i ennill ysgoloriaethau PhD wedi eu hariannu yn codi yn aml drwy gydol y flwyddyn, ac yn cael ei hysbysebu fel cyfleoedd penodol sydd yn gofyn i chi wneud cais ffurfiol. Mae’r broses gwneud cais ar gyfer ysgoloriaethau PhD wedi eu hariannu yn amrywio o ysgol i ysgol felly mae gofyn i chi edrych ar wefan yr ysgol academaidd briodol a dilyn y cyfarwyddiadau sydd ar gael yno. Os ydych yn ansicr o unrhyw ran o’r broses gneud cais, gallwch gysylltu â’r ysgol academaidd briodol yn uniongyrchol am gyngor neu gallwch e-bostio postgraduatestudy@bangor.ac.uk

Gallwch nawr wneud cais ar-lein ar gyfer holl raglenni ôl-raddedig trwy ddysgu a rhaglenni ymchwil ôl-raddedig y Brifysgol (gan eithrio TAR, Diploma mewn Therapi Galwedigaethol a DClinPsy).

Myfyrwyr Cartref/UE

Gwneud cais ar-lein

Gwneud cais ar-lein

Gyda phwy yr wyf angen cysylltu?

Am wybodaeth bellach neu gyngor am wneud cais, cysylltwch â'r Swyddfa Derbyniadau Ôl-raddedig

E-bost: postgraduate@bangor.ac.uk
Ffôn: (01248) 383717

Myfyrwyr Rhyngwladol

Pryd i wneud cais

Bydd y Brifysgol yn derbyn ceisiadau drwy gydol y flwyddyn ond byddwn yn gyffredinol yn eich annog i anfon eich cais cyn diwedd mis Mehefin. Mae hyn yn rhoi cyfle i chi wneud trefniadau ariannol a/neu lety ac i chi fedru cael gafael ar drawsgrifiadau a geirda os nad ydych wedi eu hanfon gyda’r cais gwreiddiol.

Mwy o Wybodaeth

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