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), and in Grenoble (IGE). The PhD candidate will be associated with the targeted ISClim project (Polar Ice Sheets in the Climate System – addressing high-end sea-level scenarios) of TRACCS (https://pepr
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to the understanding of climate change and its consequences. The climate effect and the ability of mixed-phase clouds to form precipitation is strongly dependent on the presence of ice crystals. Observations show that
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of the Hub. Our approach enhances T2 (Interconnected QC systems) through verification methods for connected networks, supports T1 (Integrated quantum demonstrators) via hardware-agnostic metrics, and enables
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Deadline: 30 September 2025 A fully funded four-year PhD position is available to work on the project titled “Real-world quantum verification and benchmarking of noisy hardware”. This position is a
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Deadline: 31 August 2025 A fully funded four-year PhD position is available to work on the project titled “Real-world quantum verification and benchmarking of noisy hardware”. This position is a
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of mixed-phase clouds to form precipitation. This depends largely on the presence of ice crystals. In a preliminary study, we were able to show that long-chain carbohydrates (polysaccharides) produced by
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the interface between formal verification and automated planning. This is a unique opportunity to contribute to safer, more intelligent systems through a combination of theoretical work and practical
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Everyone is talking about artificial intelligence. But who is developing the necessary chips? We are, for example! Would you like to help drive the development of a new highly efficient AI hardware platform as a doctoral student? At Fraunhofer IPMS , in collaboration with renowned German and...
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of IC design with a focus on new architectures of CMOS backplanes. What you will do Developing, implementing and experimentally testing concepts for CMOS backplanes for OLED microdisplays Designing analog
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. Investigation of the unique year-round Rothera CO2 timeseries (2010-2020) has highlighted how wintertime sea ice cover controls CO2 uptake by Antarctic coastal waters [1]. Rapid sea ice decline, strong glacial