Change of phase for the humid atmosphere
Duration: 47 mins 50 secs
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About this item
| Description: |
Temam, RM (Indiana University)
Tuesday 03 December 2013, 10:15-11:00 |
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| Created: | 2013-12-06 16:41 |
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| Collection: | Mathematics for the Fluid Earth |
| Publisher: | Isaac Newton Institute |
| Copyright: | Temam, RM |
| Language: | eng (English) |
| Distribution: |
World
(downloadable)
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| Explicit content: | No |
| Aspect Ratio: | 16:9 |
| Screencast: | No |
| Bumper: | UCS Default |
| Trailer: | UCS Default |
| Abstract: | 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. |
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