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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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Description The researcher will use modeled surface ocean microplastic abundances and improved sea-spray-based emission functions to represent ocean–atmosphere transfer processes. Using the GEOS-Chem global
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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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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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water and likely to harbor a liquid ocean beneath their icy crust. The internal dynamics of these systems remain largely unknown, particularly the main sources of oceanic and heat movements, and the
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on solubility, dissolution kinetics, and microbial influences. Your work will refine global carbon cycle models, enhance CO₂ sequestration understanding, and position you at the forefront of ocean
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waves from shots). The postdoctoral researcher will use data acquired in Ecuador on a 3D network of ocean bottom seismometers and land stations. As part of Mission 1: 1. Implementation/adaptation
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together with the new numerical model to compare cooling rates in the various available sections of oceanic crust. These, together with new data from natural samples from selected areas, will be used
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particular the hypothesis that the models applied to convert ALS measurements into above-ground biomass are transferable to all Central African forest landscapes, and the hypothesis that the BIOMASS satellite
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-frequency signals, which largely come from thermal variations at the ocean floor related to the circulation of water masses. 2. Apply fine physical models in order to better understand, characterize and