Using systematic multiscale asymptotics, Majda and Klein arrived at an asymptotic closure for the ideal fluid equations governing dynamics on large scales in the tropical atmosphere. In collaboration with Majda, we considered a plausible model for smaller scale flows in the tropics and are able to calculate the structure of the Madden-Julian oscillation; this is a planetary scale organization of winds,the understanding of which has been called "the holy grail" of tropical meteorology.
In a second problem, we studied the equatorial primitive
equations over longer time and spatial scales. The resultant coupled nonlinear dispersive equations for the amplitudes of interacting wave packets are novel both from the perspective of the atmospheric sciences and from a more general mathematical setting. These equations describe the influence of large scale tropical waves on midlatitude waves and, in particular, are relevant for understanding the effect of the Madden-Julian oscillation on midlatitude weather. I will also discuss the Hamiltonian structure of these waves and show that they admit some analytic solitary wave solutions.
This talk will introduce and solidify some concepts in TV Minimization via Chambolle Duality. I will also give an intro into image segmentation and talk about some recent work in this area.
A Schur function on the polydisk is just an analytic
function bounded by one in supremum norm. Motivated by a natural
interpolation problem for Schur functions, we discuss a theorem which
reproves positive results in dimensions one and two, and sheds light
on difficulties in higher dimensions.
Following in the spirit of Greg Knese's excellent talk from last quarter, I show how
some concepts in complex analysis (three lines theorem and entire
functions) were used to prove a (sharp) basic inequality in classical
Fourier analysis (Hausdorff-Young). I also show how a result of mine from 1974 in operator theory leads to that same inequality, as well as some new (at the time) inequalities on some noncommutative groups including the two dimensional ax+b group. This motivates an introduction to abstract harmonic analysis, which I survey in anticipation of future talks I am planning to give on some 21st century applications of this noncommutative theory to engineering (e.g. robotics, wavelet transforms).
In this talk, I consider the problem of finding explicit recursive for- mulas to compute the perturbed eigenvalues and eigenvectors of non- selfadjoint analytic perturbations of matrices with degenerate eigenvalues. Based on some math-physics problems arising from the study of slow light in photonic crystals, we single out a class of perturbations that satisfy what I call the generic condition. It will be shown that for this class of perturbations, the problem mentioned above of finding explicit recursive formulas can be solved. Using these recursive formulas, I will list the first and second order terms for the perturbed eigenvalues and eigenvectors of perturbations belonging to this class.
Hydraulic fractures (HF) are a class of tensile fractures that propagate in brittle
materials by the injection of a pressurized viscous fluid. In this talk I provide examples of natural HF and situations in which HF are used in industrial problems. Natural examples of HF include the formation of dykes by the intrusion of pressurized magma from deep chambers. They are also used in a multiplicity of engineering applications, including: the deliberate formation of fracture surfaces in granite quarries; waste disposal; remediation of contaminated soils; cave inducement in mining; and fracturing of hydrocarbon bearing rocks in order to enhance production of oil and gas wells. Novel and emerging applications of this technology include CO2 sequestration and the enhancement of fracture networks to capture geothermal energy.
I describe the governing equations in 1-2D as well as 2-3D models of HF, which involve a coupled system of degenerate nonlinear integro-partial differential equations as well as a free boundary. I demonstrate, via re-scaling the 1-2D model, how the active physical processes manifest themselves in the HF model and show how a balance between the dominant physical processes leads to special solutions. I discuss the challenges for efficient and robust numerical modeling of the 2-3D HF problem and some techniques recently developed to resolve these problems: including robust iterative techniques to solve the extremely stiff coupled equations and a novel Implicit Level Set Algorithm (ILSA) to resolve the free boundary problem. The efficacy of these techniques is demonstrated with numerical results.
Relevant papers can be found at: http://www.math.ubc.ca/~peirce