General Information
The aim of the course is to introduce the concepts, rationale, and
tools needed to derive and analyse mathematical models of physical phenomena.
Mathematical modelling takes place in two basic stages. The first
arises from the need of extracting a simpler mathematical description
from a physical theory which is intractable in its full generality.
This usually targets
a specific mechanism believed to be the most relevant in a certain problem
to be solved. At this stage physical insight into the phenomena to be
studied is crucial.
Once the mathematical model has been defined,
there remains the task of extracting useful information
through the analysis of its solutions.
This stage necessarily consists of a rather broad collection of tools
and techniques, in classical as well as modern mathematics, rather than
a self-consistent theory founded on a limited set of fundamental assumptions.
Because of this, mathematical modelling is best learned by first working within
the context of specific examples. However, inevitably one finds
that the experience gained within a particular application does not quite
transfer to a new problem to be solved. After studying in detail a core
set of examples, the course will therefore
emphasize unifying ideas and stress their theoretical background.
These ideas will then be tested on a set of problems close to the
current research interests of the instructor.
While the necessary physical background for all problems will be developed
from scratch in class and through independent reading, some familiarity
with the fundamentals of Fluid Mechanics is assumed. The prerequisite mathematical
tools will be at the level of those developed in the Methods of
Applied Mathematics two-semester sequence. Some more advanced
tools will be developed during the second part of the course.
Exposure to analysis of ordinary and partial differential equations
and numerical methods for scientific computing is recommended.
This course is the second semester sequel to Math 228.
Topics will be selected from the following
list:
- Classical Geophysical Fluid Flows:
- Rotating fluid flows, Coriolis effects and Taylor-Proudman Theorem.
- Shallow water equations.
- Potential vorticity, Ertel's theorem.
- Wave motions: Rossby, Kelvin, Poincaré and gravity waves.
- Hydrostatic balance: Primitive equations.
- Geostrophic and Quasigeostrophic approximations.
- The effects of stratification: Boussinesq approximation.
- Internal waves, barotropic and baroclinic instabilities.
- Rayleigh-Bénard convection.
- Modelling Examples from Current Research Projects:
- Weakly compressible Navier-Stokes flows.
- Non-Newtonian fluids: viscoelasticity and anisotropic microstructure
in polymer and liquid crystalline polymers flows.
- Multiphase porous media flows: closure of conservation equations
and simplified models.
- Atmospheric vortices: dust-devils, tornadoes, hurricanes.
- Long internal gravity wave models.
- Mixing in stratified fluids.
Textbooks:
- An Introduction to Fluid Mechanics, by G.K. Batchelor,
Cambridge University Press, London.
- Fluid Mechanics, by L.D. Landau and E.M. Lifshitz, Pergamon
Press,
Reading.
- Geophysical Fluid Dynamics, by J. Pedlosky, Springer, New York.
- Advanced Mathematical Methods for Scientists and Engineer,
by C. Bender and S. Orszag.
- Linear an Nonlinear Waves, by G.B. Whitham.
- Solitons and the Inverse Scattering Transform, by M.J. Ablowitz
and
H. Segur, SIAM, Philadelphia.
- Papers and notes provided by the instructor.
Prerequisites:
Familiarity with mathematical modelling as developed in the
first semester part Math. 228,
Methods of Applied Mathematics, Math. 198-199.
Familiarity with basic notions of scientific computing, at the level of
Math. 191-192.
The above prerequisites can be waived upon demonstration
of sufficient maturity in the theory of
ordinary and partial differential equation,
as well as fundamental concepts of fluid
mechanics.