Don't miss our weekly PhD newsletter | Sign up now Don't miss our weekly PhD newsletter | Sign up now

  Can ocean gliders improve our ocean forecast models? (HALLUENV19ARIES) [CASE project with Cefas]


   School of Environmental Sciences

This project is no longer listed on FindAPhD.com and may not be available.

Click here to search FindAPhD.com for PhD studentship opportunities
  Dr Robert Hall, Dr Jennifer Graham  No more applications being accepted  Competition Funded PhD Project (European/UK Students Only)

About the Project

This is a CASE project with Cefas.

Scientific Rationale
The shallow seas over continental shelves are an important sink in the global carbon cycle and therefore have a large impact on Earth’s climate. Despite their importance, these shelf seas are not well represented in global climate simulations. Climate models struggle to reproduce the exchange of heat, freshwater and carbon between shelf seas and the deep ocean, due to complex interactions between the processes involved. Around the European continental shelf, water typically flows onto the shelf in the surface layer, and off-shelf near the bottom. This downwelling circulation exports carbon to the deep ocean, away from the atmosphere. The processes that drive cross-shelf exchange can only be accurately simulated using regional models with grid spacings of order 1 km; coarser resolution global models, currently used to assess the carbon cycle, miss these processes. A new generation of ocean models has recently been developed that begin to resolve these shelf break processes (Graham et al., 2018). Combined with high-resolution observations from autonomous ocean gliders (e.g. Queste et al., 2016; Hall et al., 2017; Sheehan et al., 2018), there is potential for a step-change in our understanding of the physical drivers of carbon export.

Research Methodology
High-resolution ocean glider observations will be compared with output from operational ocean forecast models to determine the key processes driving cross-shelf exchange and assess model performance. The project will develop a two-way synergy between modelling and observations, with simulations informing glider mission planning as well as real-time operations, and observations informing model simulation weaknesses.

Advanced Training
You will be trained in numerical modelling of dynamic ocean processes and advanced methods for data processing, analysis and visualisation. You will participate in a research cruise, gaining experience in observational oceanographic methods, and as part of the UEA Glider Group (www.ueaglider.uea.ac.uk) be involved with the deployment and piloting of gliders during upcoming campaigns.

Person Specification
The ideal candidate will have a physical science degree or similar (e.g., oceanography, meteorology, physics, environmental sciences, engineering, mathematics; 2.1 or above). Experience with computer programming languages (e.g. Matlab, Python) will be an advantage. A background in ocean science is not required.

Start Date: October 2019
Mode of Study: Full-time or Part-time
Studentship length: 3.5 years
Minimum entry requirement: UK 2:1




Funding Notes

This project has been shortlisted for funding by the ARIES NERC Doctoral Training Partnership. Undertaking a PhD with ARIES will involve attendance at training events.
ARIES is committed to equality & diversity, and inclusion of students of any and all backgrounds.
Applicants from quantitative disciplines with limited environmental science experience may be considered for an additional 3-month stipend to take appropriate advanced-level courses. Usually only UK and EU nationals who have been resident in the UK for 3 years are eligible for a stipend. Shortlisted applicants will be interviewed on 26th/27th February 2019.

Further information: www.aries-dtp.ac.uk or contact us: [Email Address Removed]



References

1. Graham, J. A., E. O’Dea, J. Holt, J. Polton, et al., 2018: AMM15: a new high-resolution NEMO configuration for operational simulation of the European north-west shelf, Geoscientific Model Development, 11, 681–696, doi:10.5194/gmd-11-681-2018.
2. Hall, R. A., T. Aslam, and V. A. I. Huvenne, 2017: Partly standing internal tides in a dendritic submarine canyon observed by an ocean glider. Deep-Sea Research Part I, 126, 73–84, doi:10.1016/j.dsr.2017.05.015.
3. Queste, B. Y., L. Fernand, T. D. Jickells, K. J. Heywood, and A. J. Hind, 2016: Drivers of summer oxygen depletion in the central North Sea, Biogeosciences, 13, 1209–1222, doi:10.5194/bg-13-1209-2016, 2016.
4. Sheehan, P. M. F., S. L. Hughes, B. Berx, A. Gallego, R. A. Hall, K. J. Heywood, and B. Y. Queste, 2018: Shelf sea tidal currents and mixing fronts determined from ocean glider observations. Ocean Science, 14, 225–236, doi:10.5194/os-14-225-2018.


Where will I study?