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to the deep ocean. These canyons are the conduits for transport of land-derived materials to the ocean floor in avalanche-like events called turbidity currents. Turbidity currents transport enormous amounts
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PhD position on Modelling of turbidity current fluxes in submarine canyons Faculty: Faculty of Geosciences Department: Department of Earth Sciences Hours per week: 36 to 40 Application deadline
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3rd August 2026 Languages English English English We are looking for a PhD Candidate in Multi-scale, -physics, -fidelity wind modelling for wind farms Apply for this job See advertisement This is
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involves modelling wind flow across various spatial and temporal scales to improve accuracy. It aims to combine small-scale atmospheric phenomena, such as turbulence, with larger-scale weather patterns and
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Inria, the French national research institute for the digital sciences | Rennes, Bretagne | France | about 2 months ago
Reynolds transport theorem.From this modelling principle, stochastic equivalents of the classical geophysical flow models can be defined. A set of models ranging from multi-layers quasi-geostrophic models
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Inria, the French national research institute for the digital sciences | Rennes, Bretagne | France | about 2 months ago
studies in developing flow models that incorporate noise to account for modelling uncertainties or errors. The introduction of noise into ocean dynamics models must be done on a theoretically rigorous
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? Not funded by a EU programme Is the Job related to staff position within a Research Infrastructure? No Offer Description The activity aims to develop a model of a Vanadium Redox Flow Battery (VRFB
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1st August 2026 Languages English English English We are looking for a PhD Candidate within Integration of Justice and Socio-Environmental Risks into Wind-to-Hydrogen Energy Modeling Apply
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organisations and governments. As a Senior Research Associate in Sediment Flow Modelling you will extend an existing model of sediment flow dynamics on subaerial topography to create a new predictive model for
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possible to assess quantitatively which glaciers have the potential to collapse. In this context, physical ice flow modeling could be used to evaluate the current and future stability of specific glaciers in