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Nonlinear Dynamics and PDE Mini-Conference
Fall,
2007
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Monday November 19, 2007 at Arizona State University
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Schedule
Abstracts
Alp Eden, Department of Mathematics, Bogazici University:
In this talk I will review some of the work done jointly with
C. Babaoglu, S. Erbay, H. Erbay, G. Muslu, I. A. Topaloglu and E. Kuz
on the generalized Davey-Stewartson equations in the purely elliptic
case. I will cast these equations as a Nonlinear Schroedinger Equation
(NLS) with cubic like non-local non-linearity in 2D and discuss some
of the conserved quantities and their relation to the global existence
of solutions; virial identity and its relation with blow-up of
solutions ; the pseudoconformal invariance and its relation with the
time asymptotics of solutions. I will also review the on-going work on
the existence and uniqueness of solutions for NLS equations with
non-local terms on various Sobolev spaces in the spirit of
Kato's[1987] work for NLS.
Luan Thach Hoang, School of Mathematics, University of Minnesota:
We study the asymptotic behavior of the statistical solutions to the
3D Navier-Stokes equations using a normalization map developed by
Foias and Saut. It is then applied to the study of mean energy, mean
dissipation rate of energy, and mean helicity of the spatial periodic
flows driven by potential body forces. The statistical distribution of
the asymptotic Beltrami flows are also investigated. We connect our
mathematical analysis with the empirical theory of decaying
turbulence. With appropriate mathematically defined ensemble averages,
the Kolmogorov universal features are shown to be transient in
time. We provide an estimate for the time interval in which those
features may still be present.
Igor Kukavica, Department of Mathematics, USC:
TBA
Pablo Padilla, Department of Mathematics, University of Mexico:
We consider dynamical systems generated by ordinary and partial
differential equations. By studying area functionals in phase space,
we formulate variational principles in order to determine the
existence of particular invariant sets. These can also be implemented
numerically and several applications to heteroclinic and periodic
orbits are presented.
Edriss Titi, Department of Mathematics, U.C. Irvine:
The basic problem faced in geophysical fluid dynamics is
that a mathematical description based only on fundamental physical
principles, the so-called the ``Primitive Equations'', is often
prohibitively expensive computationally, and hard to study
analytically. In this talk I will survey the main obstacles in
proving the global regularity for the three-dimensional
Navier--Stokes equations and their geophysical counterparts. Even
though the Primitive Equations look as if they are more difficult to
study analytically than the three-dimensional Navier--Stokes
equations I will show in this talk that they have a unique global
(in time) regular solution for all initial data.
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