University College London Featured PhD Programmes
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Climatology & Climate Change (3d) PhD Projects, Programs & Scholarships

We have 10 Climatology & Climate Change (3d) PhD Projects, Programs & Scholarships

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  NERC-funded PhD studentships: Department of Earth Science and Engineering, Imperial College London

Funding Type

PhD Type

The Science and Solutions for a Changing Planet (SSCP) Doctoral Training Partnership integrates six host partners and a number of business and policy sector partners, to offer an exciting programme that trains and inspires the next generation of environmental experts and leaders to tackle some of the toughest challenges of our time.
  Depositional architecture and deformation of an active interbasinal relay zone: Corinth Isthmus, Greece
  Dr R Collier, Prof DM Hodgson
Application Deadline: 6 January 2020

Funding Type

PhD Type

Relay zones in active rifts are areas where strain is distributed between overlapping normal faults. At the scale of the major basin-bounding faults, interbasinal relay zones (or accommodation zones) separate depocentres along the rift axis.
  SCENARIO - Developing an urban canopy model for improved weather forecasts in cities
  Research Group: SCENARIO NERC DTP
  Prof J Barlow, Dr O Coceal, Dr M Carpentieri
Application Deadline: 24 January 2020

Funding Type

PhD Type

Most of the world’s population now experiences an urban version of weather extremes and climate change. Accurate forecasting of weather and air quality in cities relies on correctly representing the physics of turbulent exchange between the surface and the overlying atmosphere.
  Closing loopholes in the nitrogen cycle: Nitrification now and in the future
  Dr A Yool, Prof T Tyrrell, Dr A Martin, Prof N Bates
Application Deadline: 3 January 2020

Funding Type

PhD Type

Project Rationale. Nitrification ( oxidation) of ammonia (NH3) back to nitrate (NO3-) is an important regenerative step in the nitrogen cycles of both marine and terrestrial systems.
  Arctic sea-ice decline: An ‘opening’ for more wind energy input to the ocean?
  Dr Y Lenn, Dr T Rippeth
Application Deadline: 17 January 2020

Funding Type

PhD Type

Arctic summers are now characterized by ever-expanding areas of open water exposed by the declining sea ice. This dramatic decline has input fresh meltwater to the surface ocean and created more openings for direct exchange of heat, freshwater and momentum (i.e.
  Microplastic-sediment interactions (MiPSi)
  Research Group: Earth Surface Science
  Dr K Spencer, Prof G Wharton
Applications accepted all year round

Funding Type

PhD Type

The accelerating global release of microplastics (mP) into the aquatic environment seems inevitable, with long-term consequences for water quality and biodiversity.
  Quantifying the contribution of enhanced carbonate weathering to Earth system resilience. PhD in Geography (NERC GW4+ DTP)
  Prof T Lenton
Application Deadline: 6 January 2020

Funding Type

PhD Type

Lead Supervisor. Prof Tim Lenton, Department of Geography, College of Life and Environmental Sciences, University of Exeter. Additional Supervisors.
  How can forests help the UK move towards net-zero greenhouse gas emissions?
  Dr C Scott, Dr S Arnold, Prof P Forster
Application Deadline: 6 January 2020

Funding Type

PhD Type

In order to limit warming to 1.5 degrees Celsius above the pre-industrial period, global carbon dioxide emissions must reach net-zero by around the middle of the 21st century and become negative thereafter [1].
  A big data virtual investigation of chemistry in the upper troposphere
  Dr E Marais
Application Deadline: 29 January 2020

Funding Type

PhD Type

The global upper troposphere (8-12 km overhead) is a profoundly important part of the atmosphere that impacts climate, air quality and the chemical composition of the atmosphere.
  Testing the links between magmatic, tectonic and climate controls on hydrothermal activity at the Mid-Atlantic Ridge
  Dr A Lichtschlag, Dr B Murton, Prof R James
Application Deadline: 3 January 2020

Funding Type

PhD Type

Project Rationale. High temperature hydrothermal activity at mid-ocean ridges is driven mainly by magmatic heat and crystallization and responds to structural processes that open-up and maintain fluid pathways from the interior of the ocean crust to the seafloor.
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