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Change of phase for the humid atmosphere

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If you have a question about this talk, please contact Mustapha Amrani.

Mathematics for the Fluid Earth

In this lecture we will recall the atmospheric equations of water vapor with saturation. In their simplest form, these equations form a nonlinear system of partial differential equations with discontinuities. We will address the issue of the modelling of the system in the presence of singularities, and some questions on the existence, uniqueness and regularity of these solutions.

This talk is part of the Isaac Newton Institute Seminar Series series.

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