Seminars and Colloquia by Series

Mean viability and 2nd-order Hamilton-Jacobi-Bellman equations

Series
PDE Seminar
Time
Tuesday, November 12, 2024 - 15:30 for 1 hour (actually 50 minutes)
Location
Skiles 006
Speaker
Christian KellerUniversity of Central Florida
I present a new approach of proving uniqueness for viscosity solutions of fully nonlinear 2nd-order Hamilton-Jacobi-Bellman equations. 
This approach is purely probabilistic. It uses the concept of mean viability and the closely related notion of quasi-contingent solution. 
Unlike all existing methods in the literature, my approach does not rely on finite-dimensional results. 
This is of relevance for genuinely infinite-dimensional open problems.

 

Concave foliated flag structures and Hitchin representations in SL(3,R) by Max Riestenberg

Series
Geometry Topology Seminar
Time
Monday, November 11, 2024 - 14:00 for 1 hour (actually 50 minutes)
Location
Skiles 006
Speaker
Max RiestenbergMax Plank Institute for Mathematics in the Sciences

In 1992 Hitchin discovered distinguished components of the PSL(d,R) character variety for closed surface groups pi_1S and asked for an interpretation of those components in terms of geometric structures. Soon after, Choi-Goldman identified the SL(3,R)-Hitchin component with the space of convex projective structures on S. In 2008, Guichard-Wienhard identified the PSL(4,R)-Hitchin component with foliated projective structures on the unit tangent bundle T^1S. The case d \ge 5 remains open, and compels one to move beyond projective geometry to flag geometry. In joint work with Alex Nolte, we obtain a new description of the SL(3,R)-Hitchin component in terms of concave foliated flag structures on T^1S. 

Regularized Stein Variational Gradient Flow

Series
Applied and Computational Mathematics Seminar
Time
Monday, November 11, 2024 - 14:00 for 1 hour (actually 50 minutes)
Location
Skiles 005 and https://gatech.zoom.us/j/94954654170
Speaker
Ye HeGeorgia Tech

The stein variational gradient descent (SVGD) algorithm is a deterministic particle method for sampling. However, a mean-field analysis reveals that the gradient flow corresponding to the SVGD algorithm (i.e., the Stein Variational Gradient Flow) only provides a constant-order approximation to the Wasserstein gradient flow corresponding to the KL-divergence minimization. In this work, we propose the Regularized Stein Variational Gradient Flow, which interpolates between the Stein Variational Gradient Flow and the Wasserstein gradient flow. We establish various theoretical properties of the Regularized Stein Variational Gradient Flow (and its time-discretization) including convergence to equilibrium, existence and uniqueness of weak solutions, and stability of the solutions. We provide preliminary numerical evidence of the improved performance offered by the regularization.

Enumeration of special divisors on graphs

Series
Algebra Seminar
Time
Monday, November 11, 2024 - 11:30 for 1 hour (actually 50 minutes)
Location
Skiles 005
Speaker
Nathan PfluegerAmherst College

Please Note: There will be a pre-seminar at 10:55 am.

Young tableaux arise in the enumerative geometry of linear series on curves in formulas for the Chow class and the holomorphic Euler characteristic of Brill--Noether varieties. I will discuss an intriguing tropical generalization of these two facts: the formulas for Chow class and Euler characteristic of Brill--Noether loci on a general curve occur in the first and last terms of the Ehrhart polynomial of the tropical Brill--Noether loci on a chain of loops. I will speculate on some generalizations and algebraic analogs of this calculation.

Some open problems concerning the dynamics of Earth’s ice sheets

Series
CDSNS Colloquium
Time
Friday, November 8, 2024 - 15:30 for 1 hour (actually 50 minutes)
Location
Skiles 314
Speaker
Alex RobelGeorgia Tech

Ice sheets are fascinating dynamical systems that flow, fracture and melt on a wide range of time scales, presenting a range of challenging prediction problems with important implications for how coastal communities plan for sea level rise. In this talk, I will introduce a few outstanding problems concerning the evolution of Earth’s ice sheets under climate change. I will start by introduce the classical theory of “marine ice sheet instability” which describes how glacier ice flows from the land to ice which floats on the ocean, and leads to a saddle-node bifurcation in ice sheet size under climate change. Many contemporary predictions of ice sheet change hold that such a bifurcation is currently unfolding at a number of glaciers in Greenland and Antarctica and could lead to runaway ice sheet retreat even if global temperatures stop increasing in the future. I discuss our recent work on whether this bifurcation may actually play out as a sliding-crossing bifurcation, and the role of a stochastic climate system in driving the system through this bifurcation where nonlinearities cause evolution of the leading order moments of the distribution of glacier state.

Graph decompositions, Ramsey theory, and random graphs

Series
Combinatorics Seminar
Time
Friday, November 8, 2024 - 15:15 for 1 hour (actually 50 minutes)
Location
Skiles 005
Speaker
Yuval WigdersonETH Zürich

A basic result of probabilistic combinatorics, originally due to Erdős and Rényi, is the determination of the threshold at which the random graph $G_{n,p}$ contains a triangle with high probability. But one can also ask more refined versions of this question, where we ask not just for one triangle but for many triangles which interact in complicated ways. For example, what is the threshold at which we can no longer partition $G_{n,p}$ into two triangle-free subgraphs?


In this talk, I will discuss the proof of the Kohayakawa–Kreuter conjecture, which gives a general answer to all such questions. Rather surprisingly, a key step of the proof is a purely deterministic graph decomposition statement, closely related to classical results such as Nash-Williams' tree decomposition theorem, whose proof uses techniques from combinatorial optimization and structural graph theory.

Based on joint works with Micha Christoph, Eden Kuperwasser, Anders Martinsson, Wojciech Samotij, and Raphael Steiner.

Taking a trip to moiré land: Foundations of moiré phonons

Series
Math Physics Seminar
Time
Friday, November 8, 2024 - 11:00 for 1 hour (actually 50 minutes)
Location
Clough 280
Speaker
Michael HottUniversity of Minnesota Twin Cities

As highly tunable platforms with exotic rich phase diagrams, moiré materials have captured the hearts and minds of physicists. Moiré materials arise when 2D crystal layers are stacked at relative twists. Their almost periodicity and multiscale behavior make these materials particularly mathematically appealing. We will describe the challenges in establishing a framework to study (phonon/vibrational) wave propagation in these materials, and explain how to overcome them.

Distance theorems and the smallest singular value of inhomogeneous random rectangular matrices

Series
Stochastics Seminar
Time
Thursday, November 7, 2024 - 15:30 for 1 hour (actually 50 minutes)
Location
Skiles 006
Speaker
Manuel FernandezGeorgia Tech

In recent years, significant progress has been made in our understanding of the quantitative behavior of random matrices. Such results include delocalization properties of eigenvectors and tail estimates for the smallest singular value. A key ingredient in their proofs is a 'distance theorem', which is a small ball estimate for the distance between a random vector and subspace.  Building on work of Livshyts and Livshyts, Tikhomirov and Vershynin, we introduce a new distance theorem for inhomogeneous vectors and subspaces spanned by the columns of an inhomogeneous matrix. Such a result has a number of applications for generalizing results about the quantitative behavior of i.i.d. matrices to matrices without any identical distribution assumptions. To highlight this, we show that the smallest singular value estimate of Rudelson and Vershynin, proven for i.i.d. subgaussian rectangular matrices, holds true for inhomogeneous and heavy-tailed matrices.
This talk is partially based on joint work with Max Dabagia.

Integer distance sets

Series
School of Mathematics Colloquium
Time
Thursday, November 7, 2024 - 11:00 for 1 hour (actually 50 minutes)
Location
Skiles 005
Speaker
Rachel GreenfeldNorthwestern University

A set in the Euclidean plane is called an integer distance set if the distance between any pair of its points is an integer.  All so-far-known integer distance sets have all but up to four of their points on a single line or circle; and it had long been suspected, going back to Erdős, that any integer distance set must be of this special form. In a recent work, joint with Marina Iliopoulou and Sarah Peluse, we developed a new approach to the problem, which enabled us to make the first progress towards confirming this suspicion.  In the talk, I will discuss the study of integer distance sets, its connections with other problems, and our new developments.
 

Bounds for bilinear averages and its associated maximal functions

Series
Analysis Seminar
Time
Wednesday, November 6, 2024 - 14:00 for 1 hour (actually 50 minutes)
Location
Skiles 005
Speaker
Tainara Gobetti BorgesBrown University

Let $S^{2d-1}$ be the unit sphere in $\mathbb{R}^{2d}$, and $\sigma_{2d-1}$ the normalized spherical measure in $S^{2d-1}$. The (scale t) bilinear spherical average is given by 
$$\mathcal{A}_{t}(f,g)(x):=\int_{S^{2d-1}}f(x-ty)g(x-tz)\,d\sigma_{2d-1}(y,z).$$
There are geometric motivations to study bounds for such bilinear spherical averages, in connection to the study of some Falconer distance problem variants. Sobolev smoothing bounds for the operator 
$$\mathcal{M}_{[1,2]}(f,g)(x)=\sup_{t\in [1,2]}|\mathcal{A}_{t}(f,g)(x)|$$
 are also relevant to get bounds for the bilinear spherical maximal function
$$\mathcal{M}(f,g)(x):=\sup_{t>0} |\mathcal{A}_{t}(f,g)(x)|.$$
In a joint work with B. Foster and Y. Ou, we put that in a general framework where $S^{2d-1}$ can be replaced by more general smooth surfaces in $\mathbb{R}^{2d}$, and one can allow more general dilation sets in the maximal functions: instead of supremum over $t>0$, the supremum can be taken over $t\in \tilde{E}$ where $\tilde{E}$ is the set of all scales obtained by dyadic dilation of fixed set of scales $E\subseteq [1,2]$.

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