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is to investigate the seismological manifestation of contrasting modes seafloor spreading regimes across the global mid-ocean ridge system. This will involve a systematic re-analysis of mid-ocean ridge
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to investigate the parameters that control the triggering, speed and geometry of magmatic intrusion events at mid-ocean ridges, using dynamical models constrained with seismo-geodetic observations
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systems, specifically air-sea interactions in the ocean. The primary objective is to develop a consistent and well-calibrated mixed-layer-wave parameterization to capture turbulent kinetic energy (TKE) and
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superconducting qubits to state-of-the-art quantum limited amplifiers. Your main task will be to build devices such as non-reciprocal amplifiers operating close to the quantum limit, taking advantage of our
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variations over time. The energy efficiency of the solution will have to be evaluated at the level of the entire life cycle of a data center. The final objective is to use these mechanisms with sobriety in
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approaches and, therefore, understand variation of tree functioning at the site. - Geophysical data acquisition using Electromagnetic Induction (EMI) and Electrical Resistivity Tomography (ERT) at Paracou
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sensitivity of OECT is crucial. Multi-variate data analysis on co-integrated multi-materials micro-sensor array will be performed. Although the methodology is generic and low cost, the main challenge will lie
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through the EU Research Framework Programme? Not funded by a EU programme Is the Job related to staff position within a Research Infrastructure? No Offer Description In the context of MUSH-OCEAN, this
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the Laboratory of Planetology and Geosciences, CNRS UMR 6112, in Nantes, France. Our research aims to study the impact of heterogeneous heat flux at the core-mantle boundary (CMB) on dynamo regimes (dipole
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Biol - Morand G et al (2024) Predicting species distributions in the open ocean with convolutional neural networks. Peer Community J Main activities (in chronological order): - Familiarise oneself with