Dynamique des fluids
Org:
Serge D’Alessio (Waterloo),
J.P. Pascal (Ryerson) et
Katrin Rohlf (Ryerson)
[
PDF]
 JAHRUL ALAM, Memorial University of Newfoundland
A multiscale methodology for simulating the atmospheric boundary layer. [PDF]

The study of turbulence in the atmospheric boundary layer (ABL) is an important topic to the field of weather forecasting or projecting climate change. In a large eddy simulation (LES) model of the turbulent ABL, one calculates “grid scale” large eddies, where “subgrid scale” small eddies are parameterized. Evidences from physical and numerical models indicate that the LES model does not address fully the multiscale and intermittent character of the turbulent ABL. In this talk, I will present a novel “multiscale computational methodology” for modelling the full range of turbulent eddies, where a subrange of large significant eddies are calculated on a multiscale grid, and that of small nonsignificant eddies are parameterized. First, to model the full range of eddies, a multiscale representation of the mean conservation laws are derived, taking into account the surface roughness. Second, two stages of multiscale computational methods are developed. I will explain recent progresses for addressing some of the challenges that must be overcome, and will discuss possible ways for addressing other challenges, which is an ongoing research topic. I will present validation results for simulating a neutrally stable turbulent ABL using only about $41\,131$ grid points at a resolution $2\,048^3$.
 DAVID AMUNDSEN, Carleton University
Asymptotic Solutions for Resonant Acoustic Oscillations in Cylindrical and Spherical Geometries [PDF]

The propagation of acoustic waves in closed containers provides a natural context in which
to study the mechanisms of shock formation and their dependence upon underlying geometry.
As is well known, for the
case of a gas in a straight tube with a closed end, shocks form and all harmonics are generated,
see Chester (JFM 1964). Recent studies have shown that in more general axisymmetric geometries
the flow can be continuous or shocked depending on the input Mach number and the
details of the geometric configuration. A nonlinear geometric
acoustics approach is used to analyse the shocked motion of the gas and provide an
approximation with respect to a geometric parameter associated with the ratio of the inner
radius to gap width. Based
on comparisons with full numerical solutions it is seen that the approximation remains
valid for a surprisingly wide parameter regime. This provides insight into the nature
of the interplay between geometric and nonlinear effects and in particular the
transition between shocked and continuous flows. The effect of density variation
will also be discussed. This is joint work with Brian R. Seymour(UBC) and Michael P.
Mortell (UC Cork).
 JOHN BOWMAN, University of Alberta
Pseudospectral Reduction of Incompressible TwoDimensional Turbulence [PDF]

Spectral reduction was originally formulated entirely in the wavenumber
domain as a binaveraged wavenumber convolution in which bins of modes
interact with enhanced coupling coefficients. A Liouville theorem leads to
inviscid equipartition solutions when each bin contain the same number of
modes. We describe a pseudospectral implementation of spectral
reduction which enjoys the efficiency of the fast Fourier transform.
The model compares well with full pseudospectral simulations of the
twodimensional forceddissipative energy and enstrophy cascades.
 LUCY CAMPBELL, Carleton University
Generation of internal gravity waves by convection [PDF]

Internal gravity waves affect the general circulation of the atmosphere and hence it is important to understand their generation, propagation and interactions in order to represent them correctly in weather prediction and climate models. The primary mechanisms for gravity wave generation are convection in the lower atmosphere and topography. Convection is the movement of fluid particles from one location to another and it occurs in the atmosphere when the rate at which the temperature decreases with height exceeds a certain value. The mechanisms for the generation of internal gravity waves by convection are not fully understood. Investigations into these mechanisms generally involve largescale simulations using general circulation models and gravity wave drag parameterizations. However, the high level of complexity of general circulation models and the large number of degrees of freedom involved make it complicated to identify and quantify relationships between the gravity waves and the convection. A mathematical study based on relatively simple equations that can be solved either analytically or numerically would allow us to investigate these relationships directly. In this study we develop a twolayer model of internal gravity waves over convective vortices and use weaklynonlinear analyses and numerical simulations to obtain approximate solutions and investigate some of the current hypotheses for convective generation mechanisms.
 GEORGES DJOUMNA, University of Waterloo
Comparison of a range of turbulence schemes for thermally stratified lakes [PDF]

In stratified lakes the vertical mixing processes are small, as
evidenced by the small seasonal change in the hypolimnion temperature found in mid and highlatitude lakes like the Great Lakes. The basinscale internal wave field appears to be the fundamental control mechanism for the
cascade of energy from the wind into mixing and benthic boundary layer (BBL) transport. Mixing in the metalimnion and the BBL is crucial to the vertical flux of nutrients and oxygen.
In this talk a comparison of the Massachusetts Institute of Technology General Circulation Model (MITgcm) and the General Estuarine Transport Model (GETM) to an extensive set of time
series and spatially resolved measurements of Lake Erie,
with particular emphasis on appropriate parametrization
schemes for the vertical mixing is discussed. The two approaches for the parametrization
of vertical mixing include the K profile
parametrization and the Generic Length Scale (GLS) closures. The GLS turbulence closures used for the Lake Erie setup are: the Mellor and Yamada level $2.5$, $k \epsilon$ and, $gen$ a new closure scheme developed by Umlauf and Burchard [2003].
Comparison with observations shows that
the models can reproduce the time evolution of the lake temperature reasonably well.
This is a joint work with Dr. K. G. Lamb.
 JERZY FLORYAN, University of Western Ontario
SuperHydrophobicLike Effect Created by Surface Corrugations [PDF]

Drag reduction can result from the use of surfaces with microfeatures where trapped gas bubbles reduce shear stress over part of the surface exposed to a moving liquid. This is the socalled superhydrophobic effect. The best surface topography for such effect is yet to be determined and is subject to an active search. In the current implementation this effect can be taken advantage of only in the case of liquids and requires presence of a gas phase. We are looking for creation of a similar effect using surface grooves that reduce shear either through the local flow separation or through the fluid squeezing. The available results show that the shear drag can be reduced but this effect can become practical only if the associated pressure drag can be controlled. Current understanding of this effect will be discussed.
 GREG LEWIS, UOIT
Secondary flow transitions in the differentially heated rotating annulus [PDF]

We present some results on the secondary flow transitions that occur in the differentially heated rotating annulus. In particular, we seek secondary bifurcations in a model of the annulus that uses the three dimensional NavierStokes equations in the Boussinesq approximation. The flows that may be observed after transition can be quasiperiodic, and include flows such as mixedmode and amplitude vacillating solutions. We discuss the nature of these flows and the bifurcations that lead to them. In particular, the quasiperiodic flows correspond to 2tori in phasespace and result from a bifurcation from a periodic orbit, which corresponds to a rotating wave in the annulus. We also discuss the numerical techniques used to compute the flows and bifurcations.
This is joint work with Nicolas Perinet and Lennaert van Veen.
 FRANCIS POULIN, University of Waterloo
Analyzing Spectral Fluxes in WindDriven Gyres using Wavelets [PDF]

The dynamics of winddriven gyres are complex. Energy is input at the planetary scales, it cascades downwards to smaller length scales and eventually dissipates at molecular scales. Many models have been used to study this physical problem. Recently, we have performed a series of numerical simulations of a Rotating Shallow Water model (RSW) that resolves a wider range of scales than have been previously performed (the planetary scales, the mesoscales and some aspects of the submesoscale.)
For periodic domains, computing the energy spectra and spectral fluxes is relatively straight forward using Fourier methods. This is more complicated for flows in a basin that are inherently inhomogeneous in nature. Here, we present a Wavelet based method that is advantageous over Fourier methods in that it allows for both better resolution of the large scales and furthermore provides spatially localized spectral information. These techniques show great promise and could readily be applied to better understand the dynamics of inhomogeneous flows in the world’s oceans.
 MARY PUGH, University of Toronto
Coating flows on slowly rotating cylinders [PDF]

We consider a horizontal cylinder, rotating about its center. A viscous fluid is on the outside of the cylinder, coating the cylinder as it rotates. We consider a lubrication approximation of the Navier Stokes equations for the regime in which the fluid film is relatively thin and the surface tension is relatively large. The resulting lubrication model may have no steady state, a unique steady state, or more than one steady state. Using both numerics and analysis, we consider the dynamics of this flow, including whether or not solutions can become singular in finite time. This is joint work with Marina Chugunova (University of Toronto) and Roman Taranets (University of Nottingham).
 MALCOLM ROBERTS, University of Alberta
On the Calculation of HigherOrder Convolutions [PDF]

The quadratic nonlinearity of the incompressible NavierStokes
equations is transformed into a binary convolution in Fourier space.
The compressible NavierStokes equations and equations with
higherorder nonlinear terms exhibit ternary or other highorder
convolutions when transformed into Fourier space.
If the input vectors are periodic or of infinite length, then an
$n$ary convolution is equal to $n1$ binary convolutions. However, we
show that this does not hold for the case of fixedlength
vectors. While the full $n$ary convolution for fixedlength vectors
is more computationally complex and requires more memory than
computing $n1$ binary convolutions, we demonstrate that this can be
cost can be greatly reduced by making use of implicitly padded
convolutions.
 MAREK STASTNA, University of Waterloo
Numerical Simulation of Confined Shear Instability [PDF]

The transition from laminar to turbulent flow via shear instability is one of the most widely studied problems in fluid mechanics. Beginning with the linear stability theory as encapsulated in the Taylor Goldstein equation, through analysis of secondary instability in the resulting billows and finishing in simulations of the complex, turbulent flow that results, the basic scenario is well understood. Experimentally, the classical tilted tube experiments due to Thorpe have demonstrated both the general validity of the theory and the rich, and complex phenomenology the physical world exhibits. In this talk I will revisit the shear transition using a pseudospectral numerical methodology that allows for the resolution of both the primary shear instability and the boundary layers on the confining walls. I will demonstrate how, and in what parameter regime, the presence of walls quenches threedimensionalization. In cases where three dimensionalization does occur I will discuss how vorticity is removed from the boundary layer, and during which portion of the instability the shear stresses on the wall reach their maximum value. Finally, I will briefly speculate on the implications of these simulations for the issue of sediment resuspension by boundary layer instabilities.
 BRUCE SUTHERLAND, University of Alberta
The Growth and Rise of Anelastic Internal Waves [PDF]

The diagnoses of internal wave propagation, anelastic growth and breaking in the middle atmosphere are assessed in general circulation models through heuristics based upon observations and the predictions of linear theory. Before wave breaking occurs, however, internal waves grow to moderately large amplitude and so the predictions of linear theory are drawn into question. In this talk weakly nonlinear theory is used to derive the nonlinear Schrodinger equation, which reveals that the dominant weakly nonlinear dynamics are determined by interactions between internal waves and the mean flow that they induce (their ``Stokes drift''). In particular, this predicts that hydrostatic internal waves are modulationally stable, meaning that their anelastic amplitude growth is retarded as the wavepacket nonlinearly disperses. Fully nonlinear simulations show, as a consequence, that hydrostatic waves can overturn tens of kilometers higher in the atmosphere than predicted by linear theory.
 MICHAEL WAITE, University of Waterloo
Noncascade effects in atmospheric turbulence [PDF]

The kinetic energy spectrum of the atmospheric mesoscale (scales of
101000 km) is an approximately 5/3 power law, which is remarkably
similar to the spectrum of threedimension isotropic turbulence. As a
result, attempts to explain this spectral range have been based on the
notion of a turbulent cascade. Different cascade mechanisms have been
proposed, including inertiagravity waves, stratified turbulence, and
surface quasigeostrophic turbulence. In this talk, I will present
numerical simulations of two noncascade mechanisms that may
contribute significantly to the flux of energy through the mesoscale.
The first is a highly nonlocal transfer of energy from large scales to the buoyancy scale due
to the instability of strongly stratified shear layers. The second is
the direct forcing of the mesoscale by heating from moist convection.
Implications for existing theories of the mesoscale spectrum will be
discussed.
© Société mathématique du Canada