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Exploring Double Diffusive Convection at the Earth's Core-Mantle Boundary

This research project aims to investigate the processes, composition, and temperature dynamics at the core-mantle boundary, focusing on double diffusive convection. By analyzing the mass flux at CMB and the reversal of FeO flux direction in certain models, the study also explores seismic detection techniques to further understand Earth's interior. The ultimate goals include enabling interdisciplinary research, developing a cohort of young researchers, introducing novel tools, and fostering unexpected collaborations.

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Exploring Double Diffusive Convection at the Earth's Core-Mantle Boundary

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  1. When the Mantle Meets the Core

  2. When the Mantle Meets the Core

  3. When the Mantle Meets the Core

  4. When the Mantle Meets the Core

  5. Processes Composition Temperature double diffusive convection?

  6. Model Composition Temperature Mass flux at CMB? Flux of FeO reverses direction in somemodels

  7. Seismic Detection ? Seismic Detection ?

  8. Goals of CIDER Enable interdisciplinary research and training - Builds a cohort of young researchers - Introduces researchers to new tools - Promotes new and unexpected collaborations

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