COOKIES: By using this website you agree that we can place Google Analytics Cookies on your device for performance monitoring. |
Ribbon TurbulenceAdd to your list(s) Download to your calendar using vCal
If you have a question about this talk, please contact phh1. We study geostrophic turbulence in the limit of very high bottom friction, for a two-layer model forced by a baroclinically unstable mean flow. Remarkably, the flow spontaneously self-organizes into regions of homogenized potential vorticity separated by strong, surface intensified and meandering jets (the ribbons). We interpret the emergence of these ribbons as a tendency to reach an equilibrium state of the 1-1/2 quasi-geostrophic model. The statistical mechanics theory predicts that the interface separating the regions of homogenized potential vorticity should be minimal, just like bubbles in usual thermodynamics. We argue that the ribbon dynamics result from a competition between this effect, and baroclinic instability of the jets that tends to destabilize the interface between regions of homogenized potential vorticity. This talk is part of the DAMTP Atmosphere-Ocean Dynamics series. This talk is included in these lists:
Note that ex-directory lists are not shown. |
Other listsCafe Scientifique Cambridge 3Rs seminar series King's Sustainability Series Adams Society of St John's College Cosmology lists RECOUP open seminar seriesOther talksTODAY Foster Talk - "Paraspeckles, TDP-43 & alternative polyadenylation: how regulation of a membraneless compartment guides cell fate" TBC MOVED TO 28 JUNE 2018 It takes two to tango:platelet collagen receptor GPVI-dimer in thrombosis and clinical implications Emulators for forecasting and UQ of natural hazards Roland the Hero Uncertainty Quantification with Multi-Level and Multi-Index methods |