COOKIES: By using this website you agree that we can place Google Analytics Cookies on your device for performance monitoring. |
University of Cambridge > Talks.cam > Isaac Newton Institute Seminar Series > Statistical stability arguments for maximum kinetic energy dissipation
Statistical stability arguments for maximum kinetic energy dissipationAdd to your list(s) Download to your calendar using vCal
If you have a question about this talk, please contact Mustapha Amrani. Mathematics for the Fluid Earth The hypothesis that stationary turbulent flows have maximal mean-flow kinetic energy dissipation (Max-D) is intriguing because mean-flow properties can be predicted without modelling the turbulent component of the flow. Our knowledge of Max-D is largely restricted to relatively simple laboratory flows. Measured Poiseuille flow profiles match Max-D predictions closely and, under these simplified conditions, Malkus’s statistical stability argument provides some theoretical justification for Max-D [1]. However, it is not clear whether Max-D is applicable to more complicated fluid systems, like Earth’s atmosphere [2]. Recent global climate model simulations have found that the calibrated values of important tunable parameters are indeed consistent with Max-D [3]. Furthermore, the maximum entropy framework [4], which naturally gives a Max-D principle in the case of simple laboratory flows, can be readily applied to more complicated systems. I will discuss attempts to gener alise the Malkus statistical stability argument and how this connects with maximum entropy arguments. In doing so I hope to compare the physical insights of statistical stability, which emphasises dynamical resilience to perturbations, with maximum entropy considerations, which ignore system dynamics. [1] W. V. R. Malkus. Borders of disorder: In turbulent channel ow. Journal of Fluid Mechanics, 489:185{198, 2003. [2] Richard Goody. Maximum entropy production in climate theory. Journal of the atmospheric sciences, 64(7):2735-2739, 2007. [3] Salvatore Pascale, Jonathan M. Gregory, Maarten H.P. Ambaum, and Remi Tailleux. A parametric sensitivity study of entropy production and kinetic energy dissipation using the FAMOUS AOGCM . Climate Dynamics, 38(5-6):1211-1227, 2012. [4] Dewar R and Maritan A. A theoretical basis for maximum entropy production. 2013. In Beyond the Second Law: Entropy Production and Non-equilibrium Systems (eds. R Dewar, C Lineweaver, R Niven, K Regenauer-Lieb), Springer, In Press This talk is part of the Isaac Newton Institute Seminar Series series. This talk is included in these lists:
Note that ex-directory lists are not shown. |
Other listsHolocaust Memorial Day Homerton Seminars Explore Islam Week 2013 Climate & Women - Talk and numeric exhibition Gurdon Institute TalksOther talksPicturing the Heart in 2020 CGHR Practitioner Series: Andrea Coomber, JUSTICE PROFESSIONAL REGISTRATION WORKSHOP Amphibian Evolution through Deep Time: Fossils, Genes and Regeneration Psychological predictors of risky online behaviour: The cases of online piracy and privacy Lecture Supper: James Stuart: Radical liberalism, ‘non-gremial students’ and continuing education Active bacterial suspensions: from individual effort to team work Café Synthetique: Graduate Talks! Alzheimer's talks A feast of languages: multilingualism in neuro-typical and atypical populations Prescribing step counts in type 2 diabetes and hypertension:Results of the Step Monitoring to improve ARTERial health trial |