Please share this open PhD position among your network of potential applicants.
Thank you for your help,
Hans Christian Steen-Larsen
Deadline October 6 2019 - application through the official link above.
There is a vacancy for a PhD position in modelling of Atmosphere-Cryosphere Exchange Processes and Ice Core Isotope Research at the Geophysical Institute at University of Bergen. The position is for a fixed-term period of 3 years. The position is part of the European Research Council funded Starting Grant SNOWISO.
About the project:
The open PhD position is part of the international European Research Council project SNOWISO - “Signals from the Surface Snow: Post- Depositional Processes Controlling the Ice Core isotopic Fingerprint “.
The SNOWISO project combines field observations, laboratory experiments, and coupled climate models in order to understand and quantify how the climate signal is recorded in the ice core water isotope records from Greenland and Antarctica.
The fundamental hypothesis, which the SNOWISO is working on, is that the climate signal in the ice core water isotope record is not only governed by the precipitation isotopes, but a combination of the precipitation isotope climate signal and the exchange between the snow surface and atmosphere. By being able to accurately understand and model how the variability of the climate is recorded in the ice core records from the Polar ice sheets the SNOWISO project will allow for integration of isotope-enabled General Circulation Models with ice cores. This will lead to the opportunity of retrieving more information from ice core records than just the local site temperature.
The work of the PhD candidate will specifically focus on modelling the influence of post-depositional processes on the ice core isotope record under different climate conditions in order to correctly interpret climate variability from ice cores.
The successful PhD candidate will reevaluate the physical foundations of air-snow exchange processes of water isotopes with respect to theory, measurements, and model implementation. Existing field observations and laboratory experiments will be used together with existing theory as foundation for creating and implementing a new physical understanding of the relevant processes in isotope-enabled regional and general circulation models.
The impact of improved descriptions and reduced uncertainty of molecular-level stable isotope processes during air-snow interaction will be evaluated using advanced, isotope-enabled coupled atmospheric models. Results will be assessed with regard to signals in ice core climate proxy archives from the Greenland and Antarctic Ice Sheets for different climate periods.
As a PhD, you will be part of a dynamic group at the Geophysical Institute, and you will also be affiliated with the Bjerknes Centre for Climate Research (BCCR). BCCR is the largest climate research centre in the Nordic countries and among the leading centres in Europe. The working environment is highly international with around 200 scientists from 37 countries. You will also be part of the national research school on Changing Climates in the Coupled Earth System (CHESS).
Qualifications and personal qualities:
About the research training
As a PhD candidate, you must participate in an approved educational programme for a PhD degree within a period of 3 years. A final plan for the implementation of the research training must be approved by the faculty within two months after you have commenced in the position. It is a condition that you satisfy the enrolment requirements for the PhD programme at the University of Bergen.
We can offer:
Your application must include:
For further details about the position, please contact Dr. Hans Christian Steen-Larsen, University of Bergen, [hidden email] or see https://steenlarsen.w.uib.no/
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