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Change of phase for the humid atmosphere

Temam, RM (Indiana University)
Tuesday 03 December 2013, 10:15-11:00

Seminar Room 1, Newton Institute


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.


[pdf ]


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