29,515 research outputs found

    Geodesic Flow on the Diffeomorphism Group of the circle

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    We show that certain right-invariant metrics endow the infinite-dimensional Lie group of all smooth orientation-preserving diffeomorphisms of the circle with a Riemannian structure. The study of the Riemannian exponential map allows us to prove infinite-dimensional counterparts of results from classical Riemannian geometry: the Riemannian exponential map is a smooth local diffeomorphism and the length-minimizing property of the geodesics holds.Comment: 15 page

    Energy Spectrum of Quasi-Geostrophic Turbulence

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    We consider the energy spectrum of a quasi-geostrophic model of forced, rotating turbulent flow. We provide a rigorous a priori bound E(k) <= Ck^{-2} valid for wave numbers that are smaller than a wave number associated to the forcing injection scale. This upper bound separates this spectrum from the Kolmogorov-Kraichnan k^{-{5/3}} energy spectrum that is expected in a two-dimensional Navier-Stokes inverse cascade. Our bound provides theoretical support for the k^{-2} spectrum observed in recent experiments

    Global well-posedness for the critical 2D dissipative quasi-geostrophic equation

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    We give an elementary proof of the global well-posedness for the critical 2D dissipative quasi-geostrophic equation. The argument is based on a non-local maximum principle involving appropriate moduli of continuity.Comment: 7 page

    Economic and social disparities of Romania in regional and county profile

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    Romania's accession to the European Union imposes a new way of approaching the economic and social disparities existing nowadays both at the level of the eight development regions of the country and at the level of counties as well. The analysis of the level and evolution of these disparities can be useful to all the factors that design and put into practice strategies meant to stop the gaps widening on one hand and to fill the existing gaps among the Romanian development regions on the other hand. All these analyses are made from the perspective of Romania's process of integration into the European Union's structures.convergence objective, development regions, economic disparities, EU cohesion, Principal Components Analysis.

    On a two-component π\pi-Camassa--Holm system

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    A novel π\pi-Camassa--Holm system is studied as a geodesic flow on a semidirect product obtained from the diffeomorphism group of the circle. We present the corresponding details of the geometric formalism for metric Euler equations on infinite-dimensional Lie groups and compare our results to what has already been obtained for the usual two-component Camassa--Holm equation. Our approach results in well-posedness theorems and explicit computations of the sectional curvature.Comment: 12 page

    On periodic water waves with Coriolis effects and isobaric streamlines

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    In this paper we prove that solutions of the f-plane approximation for equatorial geophysical deep water waves, which have the property that the pressure is constant along the streamlines and do not possess stagnation points,are Gerstner-type waves. Furthermore, for waves traveling over a flat bed, we prove that there are only laminar flow solutions with these properties.Comment: To appear in Journal of Nonlinear Mathematical Physics; 15 page

    Regularity of H\"older continuous solutions of the supercritical quasi-geostrophic equation

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    We present a regularity result for weak solutions of the 2D quasi-geostrophic equation with supercritical (α<1/2\alpha< 1/2) dissipation (Δ)α(-\Delta)^\alpha : If a Leray-Hopf weak solution is H\"{o}lder continuous θCδ(R2)\theta\in C^\delta({\mathbb R}^2) with δ>12α\delta>1-2\alpha on the time interval [t0,t][t_0, t], then it is actually a classical solution on (t0,t](t_0,t]

    Lagrangian-Eulerian Methods for Uniqueness in Hydrodynamic Systems

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    We present a Lagrangian-Eulerian strategy for proving uniqueness and local existence of solutions in path spaces of limited smoothness for a class of incompressible hydrodynamic models including Oldroyd-B type complex fluid models and zero magnetic resistivity magneto-hydrodynamics equations
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