Full details are available at: http://www.stcatz.ox.ac.uk/alantayler
Explosive volcanic eruptions often produce large amounts of ash that is transported high into the atmosphere in a turbulent buoyant plume. The ash can be spread widely and is hazardous to aircraft causing major disruption to air traffic. Recent events, such as the eruption of Eyjafjallajokull, Iceland, in 2010 have demonstrated the need for forecasts of ash transport to manage airspace. However, the ash dispersion forecasts require boundary conditions to specify the rate at which ash is delivered into the atmosphere.
Models of volcanic plumes can be used to describe the transport of ash from the vent into the atmosphere. I will show how models of volcanic plumes can be developed, building on classical fluid mechanical descriptions of turbulent plumes developed by Morton, Taylor and Turner (1956), and how these are used to determine the volcanic source conditions. I will demonstrate the strong atmospheric controls on the buoyant plume rise. Typically steady models are used as solutions can be obtained rapidly, but unsteadiness in the volcanic source can be important. I'll discuss very recent work that has developed unsteady models of volcanic plumes, highlighting the mathematical analysis required to produce a well-posed mathematical description.
Let $G=SL(2,\R)\ltimes R^2$ and $\Gamma=SL(2,Z)\ltimes Z^2$. Building on recent work of Strombergsson we prove a rate of equidistribution for the orbits of a certain 1-dimensional unipotent flow of $\Gamma\G$, which projects to a closed horocycle in the unit tangent bundle to the modular surface. We use this to answer a question of Elkies and McMullen by making effective the convergence of the gap distribution of $\sqrt n$ mod 1.
We study liquid crystal point defects in 2D domains. We employ Landau-de
Gennes theory and provide a simplified description of global minimizers
of Landau- de Gennes energy under homeothropic boundary conditions. We
also provide explicit solutions describing defects of various strength
under Lyuksutov's constraint.
Jakobshavn Isbrae and many other fast flowing outlet glaciers of present
and past ice sheets lie in deep troughs which often have several
overdeepened sections. To make their fast flow possible their bed needs
to be slippery which in turn means high basal water pressures. I will
present a model of subglacial water flow and its application to
Jakobshavn. I find that, somewhat surprisingly, the reason for
Jakobshavn's fast flow might be the pressure dependence of the melting
point of ice. The model itself describes the unusual fluid dynamics occurring underneath the ice; it has an interesting mathematical structure that presents computational challenges.
Turbidity currents - submarine flows of sediment - are capable of transporting particulate material over large distance. However direct observations of them are extremely rare and much is inferred from the deposits they leave behind, even though the characteristics of their source are often not known. The submarine flows of volcanic ash from the Soufriere Hills Volcano, Monsterrat provide a unique opportunity to study a particle-driven flow and the deposit it forms, because the details of the source are relatively well constrained and through ocean drilling, the deposit is well sampled.
We have formed simple mathematical models of this motion that capture ash transport and deposit. Our description brings out two dynamical features that strongly influence the motion and which have previously often been neglected, namely mixing between the particulate flow and the oceanic water and the distribution of sizes suspended by the flow. We show how, in even simple situations, these processes alter our views of how these currents propagate.
We present a variational model for the quasi-static evolution of brutal brittle damage for geometrically-linear elastic materials. We
allow for multiple damaged states. Moreover, unlike current formulations, the materials are allowed to be anisotropic and the
deformations are not restricted to anti-plane shear. The model can be formulated either energetically or through a strain threshold. We
explore the relationship between these formulations. This is joint work with Christopher Larsen, Worcester Polytechnic Institute.
We present some recent results concerning domain wall motion in one-dimensional nanowires, including the existence, velocity and stability of travelling-wave and precessing solutions. We consider the case of unixial anisotropy, characteristic of wires with symmetrical (e.g., circular) cross-section, as opposed to strongly anisotropic geometries (films and strips) that have received greater attention. This is joint work with Arseni Goussev and Valeriy Slastikov.