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with national/international collaborators from the ODUST consortium. • Access to HPC resources (e.g., IDRIS) for large-scale simulations. Where to apply Website https://emploi.cnrs.fr/Offres/CDD/UMR5299
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the OGGM glaciological model for present-day conditions and simulate the recent behavior of selected studied glaciers. • Simulate glacier behavior throughout the Holocene using available climate model
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of investigating the relationships between microstructure, processing routes, and thermomechanical performance. The research will combine physics-based modelling and numerical simulations, including thermomechanical
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of the century, which could be further amplified by a slowdown in the Atlantic Meridional Overturning Circulation (AMOC). This PhD is part of the French-Brazilian project AMACLIM (https://www.lsce.ipsl.fr/anr
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(materials, scenarios) - Translation of local knowledge into simulation rules - Facilitation or co-facilitation of model testing sessions - Collection of feedback for prototype iterations. Analysis and
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microfabrication facilities, multiphoton lithography and stereolithography systems, laboratories dedicated to the development of photocrosslinkable biomaterials, advanced optical and confocal microscopy platforms
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simulation codes such as Geant4 and/or multiscale modeling approaches will be considered an asset. Where to apply Website https://emploi.cnrs.fr/Offres/Doctorant/UMR5822-FLOJAC-103/Default.aspx Requirements
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instrumentation for the early detection of dissipation/quench, initially through voltage measurement, but other approaches (radio frequency, optical fiber, etc.) may also be considered. These developments will be
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Carlo simulations would be a plus. A good level in English (at B2 according to the Common European Framework of Reference for Languages) is required. The international, multidisciplinary and collaborative
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representation of the vertical coordinate in numerical ocean models used to simulate ocean currents, temperature, and salinity. These developments will improve the representation of deep-ocean circulation and