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paleoclimate PhD Projects, Programs & Scholarships

We have 7 paleoclimate PhD Projects, Programs & Scholarships

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  NERC Reconstructing past temperatures from the terrestrial Southern Hemisphere over the last 20,000 years
  Dr B.D.A. Naafs
Application Deadline: 7 January 2019
A NERC GW4 +DTP2 Project. Project PDF.
  The role of Antarctic sea ice in glacial-interglacial climatic transitions
  Dr Louise Sime, Dr A Marzocchi
Application Deadline: 4 January 2019
Project Rationale. Since the onset of the Northern Hemisphere glaciation, Earth’s climate has undergone large transitions between cold “glacial” and warm “interglacial” stages.
  Provenance of Southern Cape Rivers: Links to Hydroclimate and Early Humans
  Prof I Hall, Dr M Andersen
Application Deadline: 7 January 2019
Project Background. The pattern and causes of late Pleistocene climate variability in the subtropics of south-eastern Africa is intensively debated.
  E4 DTP is Edinburgh Earth, Ecology and Environment
Fully funded PhD projects addressing the most exciting. and important questions in Environmental Science.
  Tracking the ancient Indian monsoon: investigating the geochemistry of deep-sea sediments from the Bay of Bengal and Andaman Sea
  Dr K Littler, Dr B.D.A. Naafs, Prof R Pancost, Dr I Bailey
Application Deadline: 7 January 2019
This project is one of a number that are in competition for funding from the NERC Great Western Four+ Doctoral Training Partnership (GW4+ DTP).
  The Ice Age, oceans and climate: triggers of iceberg calving and rapid temperature change
  Dr R Ivanovic, Dr L Gregoire
Application Deadline: 7 January 2019
This PhD project will use climate/ice-sheet modelling to establish the complex chain of events that took place early in the last deglaciation, linking catastrophic ice sheet collapse, iceberg armadas, rapid cooling, abrupt warming and the complete reorganisation of largescale Atlantic Ocean circulation.
  Reconstructing latitudinal terrestrial environments at the Cretaceous-Palaeogene boundary; Testing the ‘Equable Earth’ hypothesis
  Dr R Jerrett, Dr B Van Dongen
Application Deadline: 6 February 2019
As anthropogenic atmospheric warming is forecasted to exceed 2°C above preindustrial temperatures by 2100, it remains unclear how thermal energy will be redistributed across the globe (from equator to pole) and to what extent this will impact the terrestrial environments.
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