Magnet.me - Het slimme netwerk waar studenten en professionals hun stage of baan vinden.
Het slimme netwerk waar studenten en professionals hun stage of baan vinden.
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Over the last five years it has become clear that the evolution of ice sheets is strongly influenced by the interaction with the ocean. This is caused by basal melting below ice shelves and by the calving of ice at the front of tide water glaciers or ice shelves. We will do this with an ice sheet model (UFEMISM) which is adaptive in space and time. The model will be tested against field observations in Greenland and used for projections of the ice sheet and thereby sea level rise for the next centuries.
Your task will be to improve an existing ice sheet model (UFEMISM) with a calving algorithm and calving law and applying this to the Greenland ice sheet. UFEMISM is a relatively new ice model with a growing user community aiming to be part of coupled Earth System Models. As such you work as part of a small group of people working on several aspects aiming to improve the role of ice sheets in climate models. This is done in the international context of ice sheet model improvements.
15% of your time will be spend to assisting with classes for Bachelor's and Master's students in (climate) physics.
Beside very good modelling skills you have to appreciate the difficulty of measuring in the field and to use these sparse field data in a smart way to validate your model. You are driven, positive and collaborative and have:
We work on a better future. In order to do that, we join forces with academics, students, alumni, social partners, the government and the corporate world. Together, we look for sustainable solutions to the big challenges of today and tomorrow.
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