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or Computer Science or equivalent with a strong desire to mathematically analyse when and how a numerical algorithm works. The PhD program in Leuven is a 4 year program. The initial contract is for one year. After nine
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cost of conventional numerical weather prediction systems, opening new possibilities for large forecast ensembles and event-based climate attribution. The PhD researcher will evaluate the predictive
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impact. Furthermore, working at AMADE is not only a professional opportunity, but also being close to a stimulating environment with all our research lines in simulation and numerical modeling
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Engineering, University of Montpellier / CNRS). This position offers a multidisciplinary environment combining structural mechanics, numerical modeling, aerodynamics, and automation, in collaboration with LIRMM
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of mountains in the global hydrological cycle? And in what happens to downstream water supply when mountains change? Do you like working with numerical models? Then this PhD might be your next step! A large part
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Parametric integrators approximate solutions of (high-dimensional) partial differential equations by restricting the numerical approximation to a closed form that nonlinearly depends on, and is
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looking to appoint a Early Stage Marie Curie Researcher to undertake high-quality research within the MSCA Doctoral Network POSEIDON (https://poseidon-dn.eu/ ). The postholder will be assisting in
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The International Institute of Molecular Mechanisms and Machines Polish Academy of Sciences | Poland | 2 days ago
and master numerous advanced experimental techniques. Furthermore, you will benefit from a young, collaborative and dynamic scientific environment. Key responsibilities: Planning and performing
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classical approaches. You will also evaluate the developed methods through numerical studies and real-time power system simulation. The research will involve scientific programming, analysis and documentation
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scales through advanced numerical modeling. Our research foci are located at both plate boundaries and within the plate interiors, inside the deep mantle and at the surface. To approach our aims, we