Higher Degree by Research Application Portal

Title
AlternativeWhat is the sedimentary signature of rapid deglaciation events?
SupervisorA/Pro Alan Aitken
KeywordsIce sheet, climate, oceans, sediments,
Research areaEarth Sciences
Project description

This PhD project will develop and apply advanced numerical approaches to analyse subglacial sediment generation under conditions of rapid deglaciation. The project will develop an approach to define the expected sedimentary output when ice sheets collapse, and to map the impact on subglacial geomorphology. The new approach will be applied to glacial catchments in past and present ice sheets and will help to constrain ice sheet evolution and projections for the future of sea level and climate. The outcomes of this project will help to understand how to characterise rapid deglaciation events in the past and identify if they are happening under present climate change.

The PhD student will:

1) Develop novel numerical workflows to model subglacial sediment generation and transport

2) Apply this to selected examples from past and present ice sheets.

3) Express these results in the context of identifying rapid ice sheet deglaciation events

Open date01 Jul 2025
Close date31 Oct 2025
SchoolSchool of Earth Sciences
Contact

alan.aitken@uwa.edu.au

Specific project requirement

The student will have a background in Earth, Cryosphere or Ocean sciences, Geomorphology or Physical Geography.

The student will be able to engage in quantitative numerical and spatial analysis methods.

Course typeDoctorates

Guidance

Earth Sciences

2025 International round open 1 July to 30 August

2025 Domestic round open 1 September to 31 October

As per Doctor of Philosophy admission criteria

Contact the supervisor for potential Masters study

What is the sedimentary signature of rapid deglaciation events?