1,532 research outputs found

    Stable self-similar blow-up dynamics for slightly L2L^2-supercritical generalized KdV equations

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    In this paper we consider the slightly L2L^2-supercritical gKdV equations ∂tu+(uxx+u∣u∣p−1)x=0\partial_t u+(u_{xx}+u|u|^{p-1})_x=0, with the nonlinearity 5<p<5+Δ5<p<5+\varepsilon and 0<Δâ‰Ș10<\varepsilon\ll 1 . We will prove the existence and stability of a blow-up dynamic with self-similar blow-up rate in the energy space H1H^1 and give a specific description of the formation of the singularity near the blow-up time.Comment: 38 page

    Standing

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    Standing

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    Local well-posedness and blow up in the energy space for a class of L2 critical dispersion generalized Benjamin-Ono equations

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    We consider a family of dispersion generalized Benjamin-Ono equations (dgBO) which are critical with respect to the L2 norm and interpolate between the critical modified (BO) equation and the critical generalized Korteweg-de Vries equation (gKdV). First, we prove local well-posedness in the energy space for these equations, extending results by Kenig, Ponce and Vega concerning the (gKdV) equations. Second, we address the blow up problem in the spirit of works of Martel and Merle on the critical (gKdV) equation, by studying rigidity properties of the (dgBO) flow in a neighborhood of solitons. We prove that when the model is close to critical (gKdV), solutions of negative energy close to solitons blow up in finite or infinite time in the energy space. The blow up proof requires in particular extensions to (dgBO) of monotonicity results for localized versions of L2 norms by pseudo-differential operator tools.Comment: Submitte

    Geosat sea-level assimilation in a tropical Atlantic model using Kalman filter

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    We present preliminary results on Geosat altimetric data assimilation in a linear vertical mode model of the tropical Atlantic Ocean. The Kalman filter technique is used to assimilate altimetric data along one track at a time as the satellite over-flies the basin. Sensitivity and validation tests have been performed with simulated data. The results obtained with Geosat data are presented and compared on a monthly basis with objective analysis of altimetric data and oceanic general circulation model results

    The representation of feedback literature in classroom observation frameworks: an exploratory study

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    Feedback is considered of great relevance for supporting student learning. It is therefore the focus of a significant body of theoretical work and is included in many observation frameworks for measuring teaching quality. However, little is currently known about the extent to which the theoretical and empirical knowledge of feedback from the literature is represented in operationalizations of feedback in observation frameworks. In this exploratory study, we first reviewed the literature and identified nine quality criteria for effective feedback. Using content analysis, we then explored the extent to which 12 widely used observation frameworks for teaching quality reflect these criteria and the similarities and differences in their approaches to capturing feedback quality. Only ten of the 12 frameworks measured feedback. Nine frameworks addressed feedback directly, while one framework only captured feedback indirectly. All frameworks differed in the number of feedback quality criteria they captured, the aspects they focused on for each one, and the detail in which they described them. One criterion (Feed Up) was not captured by any framework. The results show that more clarity is needed about which facets of feedback are integrated into frameworks and why. The study also highlights the importance of finding ways to complement observation frameworks with other measures so that feedback quality is captured in a more comprehensive fashion

    Nondispersive solutions to the L2-critical half-wave equation

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    We consider the focusing L2L^2-critical half-wave equation in one space dimension i∂tu=Du−∣u∣2u, i \partial_t u = D u - |u|^2 u, where DD denotes the first-order fractional derivative. Standard arguments show that there is a critical threshold M∗>0M_* > 0 such that all H1/2H^{1/2} solutions with ∄u∄L2<M∗\| u \|_{L^2} < M_* extend globally in time, while solutions with ∄u∄L2≄M∗\| u \|_{L^2} \geq M_* may develop singularities in finite time. In this paper, we first prove the existence of a family of traveling waves with subcritical arbitrarily small mass. We then give a second example of nondispersive dynamics and show the existence of finite-time blowup solutions with minimal mass ∄u0∄L2=M∗\| u_0 \|_{L^2} = M_*. More precisely, we construct a family of minimal mass blowup solutions that are parametrized by the energy E0>0E_0 >0 and the linear momentum P0∈RP_0 \in \R. In particular, our main result (and its proof) can be seen as a model scenario of minimal mass blowup for L2L^2-critical nonlinear PDE with nonlocal dispersion.Comment: 51 page

    Multiple-Time Higher-Order Perturbation Analysis of the Regularized Long-Wavelength Equation

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    By considering the long-wave limit of the regularized long wave (RLW) equation, we study its multiple-time higher-order evolution equations. As a first result, the equations of the Korteweg-de Vries hierarchy are shown to play a crucial role in providing a secularity-free perturbation theory in the specific case of a solitary-wave solution. Then, as a consequence, we show that the related perturbative series can be summed and gives exactly the solitary-wave solution of the RLW equation. Finally, some comments and considerations are made on the N-soliton solution, as well as on the limitations of applicability of the multiple scale method in obtaining uniform perturbative series.Comment: 15 pages, RevTex, no figures (to appear in Phys. Rev. E

    The Orbital Stability of the Ground States and the Singularity Formation for the Gravitational Vlasov Poisson System

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    International audienceWe study the gravitational Vlasov Poisson system ft+v⋅∇xf−E⋅∇vf=0f_t+v\cdot\nabla_x f-E\cdot\nabla_vf=0 where E(x)=∇xϕ(x)E(x)=\nabla_x \phi(x), Δxϕ=ρ(x)\Delta_x\phi=\rho(x), \rho(x)=\int_{\RR^N} f(x,v)dxdv, in dimension N=3,4N=3,4. In dimension N=3N=3 where the problem is subcritical, we prove using concentration compactness techniques that every minimizing sequence to a large class of minimization problems attained on steady states solutions are up to a translation shift relatively compact in the energy space. This implies in particular the orbital stability {\it in the energy space} of the spherically symmetric polytropes what improves the nonlinear stability results obtained for this class in \cite{Guo,GuoRein,Dol}. In dimension N=4N=4 where the problem is L1L^1 critical, we obtain the polytropic steady states as best constant minimizers of a suitable Sobolev type inequality relating the kinetic and the potential energy. We then derive using an explicit pseudo-conformal symmetry the existence of critical mass finite time blow up solutions, and prove more generally a mass concentration phenomenon for finite time blow up solutions. This is the first result of description of a singularity formation in a Vlasov setting. The global structure of the problem is reminiscent to the one for the focusing non linear Schrödinger equation iut=−Δu−∣u∣p−1uiu_t=-\Delta u-|u|^{p-1}u in the energy space H1(RN)H^1(\R^N)

    Continuity of the blow-up profile with respect to initial data and to the blow-up point for a semilinear heat equation

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    International audienceWe consider blow-up solutions for semilinear heat equations with Sobolev subcritical power nonlinearity. Given a blow-up point a^\hat{a}, we have from earlier literature, the asymptotic behavior in similarity variables. Our aim is to discuss the stability of that behavior, with respect to perturbations in the blow-up point and in initial data. Introducing the notion of ``profile order", we show that it is upper semicontinuous, and continuous only at points where it is a local minimum
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