Two-Dimensional and Geophysical Turbulence
Many geophysical flows are quasi-two-dimensional in nature, with motion restricted in one dimension by rotation, stratification, or physical confinement. At the most basic level, these geophysical flows can be modelled by two-dimensional fluid equations such as the two-dimensional Navier-Stokes or quasi-geostrophic equations. In regimes of small-scale pumping and weak dissipation, these systems display a flow of energy towards the largest scales, leading to a phenomenon called energy condensation at the scale of the system. This buildup of energy can induce the self-organization of the fluid flow into large-scale coherent structures that exist on top of a random turbulent background. For geophysical flows, these coherent structures usually take the form of system-sized vortices or zonal jets (think of hurricanes or large-scale ocean jets such as the Gulf Stream). Questions of universality of these structures are the most natural questions to ask for mathematicians. My interests relate to developing a statistical theory for modelling the complex interactions between the large-scale coherent structures and the underlying turbulent fluctuations.

Read More
- A. Frishman, J. Laurie and G. Falkovich, Jets or Vortices--What Flows are Generated by an Inverse Turbulence Cascade?, Phys. Rev. Fluids, 2, 032602(R), (2017)
10.1103/PhysRevFluids.2.032602
:1608.04628 - J. Laurie, G. Boffetta, G. Falkovich, I. Kolokolov and V. Lebedev, Universal Profile of the Vortex Condensate in Two-Dimensional Turbulence, Phys. Rev. Lett. 113, 254503, (2014)
10.1103/PhysRevLett.113.254503
:1406.1349


