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University of Southampton, Ocean and Earth Science Mathematics PhD Projects, Programs & Scholarships

We have 46 University of Southampton, Ocean and Earth Science Mathematics PhD Projects, Programs & Scholarships

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  Antarctica before ice sheets: polar climate history of past greenhouse worlds.
  Dr S Bohaty, Dr CD Hillenbrand, Assoc Prof R Levy, Prof P Wilson
Application Deadline: 3 January 2020

Funding Type

PhD Type

Project Rationale. During the extremely warm global ’greenhouse’ period 50 million years ago, Antarctica was mostly ice free and hosted temperate forests in coastal regions of the continent.
  Asian Monsoon drought and flood intensity: testing predicted response to changes in global warmth and polar ice volume
  Prof P Wilson, Dr C Xuan, Dr A Crocker
Application Deadline: 3 January 2020

Funding Type

PhD Type

Project Rationale. The Asian Monsoon (AM) is a major component of the global climate system, affecting the lives of four billion people.
  Avalanche dynamics on desert dunes: Processes and drivers, from ancient to modern
  Dr J Nield, Dr R Ewing, Dr M Baddock
Application Deadline: 3 January 2020

Funding Type

PhD Type

Project Rationale. Avalanching is responsible for wind-blown dune migration on Earth and Mars and because avalanches are preserved in dune stratigraphy, they are the most direct way that we can interpret past wind-climate conditions.
  Bayesian analysis of Earth’s climate sensitivity: past, present and future
  Dr P Goodwin, Dr K Oliver, Prof T Tyrrell
Application Deadline: 3 January 2020

Funding Type

PhD Type

Project Rationale. The biggest cause of uncertainty in predicting the magnitude of future global warming, for a given pattern of CO2 emissions, lies in Earth’s ‘climate sensitivity’ (the increase in average surface temperature following a sustained doubling of atmospheric carbon dioxide).
  Caribbean Subduction: Seismic Imaging of Melt and Volatiles in the Lesser Antilles with joint inversion, full-waveform, and machine learning approaches
  Dr C Rychert, Dr T Henstock
Application Deadline: 3 January 2020

Funding Type

PhD Type

Project Rationale. Dense oceanic tectonic plates sink beneath buoyant continental plates at subduction zones. The ocean plate adds volatiles like water to the mantle, lowering the melting temperature, and enabling melting and eventually creating volcanoes at Earth’s surface.
  Catastrophic change to Earth’s magnetic field
  Dr C Xuan, Prof P Wilson, Dr G Hellio
Application Deadline: 3 January 2020

Funding Type

PhD Type

Project Rationale. Earth’s magnetic field provides a protective shield from harmful effects of the solar wind, but field strength and behaviour are constantly changing.
  Challenging theories on the latitudinal coherence of the AMOC
  Dr A Sanchez-Franks, Dr E Frajka-Williams, Prof H Bryden
Application Deadline: 3 January 2020

Funding Type

PhD Type

Project Rationale. The Atlantic meridional overturning circulation (AMOC) is a large-scale oceanic circulation comprised of currents that carry warm, shallow water northwards and return cold deep-water southwards.
  Changing Ocean Freshwater and Heat Transports and Atlantic Climate Tipping Points
  Dr J Mecking, Prof S Drijfhout, Prof P Holliday
Application Deadline: 3 January 2020

Funding Type

PhD Type

Project Rationale. Abrupt climate changes can have large and devastating socio-economic impacts, therefore being able to simulate them in future climate scenarios is of great importance.
  Climate change effects on ocean biogeochemistry
  Dr S Henson, Dr A Hickman
Application Deadline: 3 January 2020

Funding Type

PhD Type

Project Rationale. Human-induced climate change is expected to affect ocean biogeochemistry through increasing temperature, ocean acidification and deoxygenation.
  Climate Change, Plate Tectonics and Machine Learning
  Dr C Rychert, Dr J Whiteside
Application Deadline: 3 January 2020

Funding Type

PhD Type

Project Rationale. Our understanding of the transition from the lithospheric plate to the weaker asthenosphere has recently been revolutionized by seismic imaging that finds a sharp, strong discontinuity at the base of the plate.
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