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) Accounting for drop size distribution variability across scales, and notably the one occurring below radar observation scales; (ii) Better understanding and quantifying the wind drift effect, i.e
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occurring below radar observation scales; (ii) Better understanding and quantifying the wind drift effect, i.e. the advection of raindrops are advected during their fall from radar observation elevations
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motional quantum ground state, which requires to monitor the motion of the particle with the highest precision possible. Typically, such monitoring is performed using a coherent (i.e. classical) light
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the production for weeks or months. Even after the production starts, it is important to track how reservoirs evolve (i.e., the quantities of remaining hydrocarbon, the flow and pressure of fluids in porous rocks
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on the potential advantages of lattices of excitons (as in Moiré superlattices). Further, we will address theoretically how exciton-exciton interactions, especially in strongly-interacting configurations (i.e