Colloquium - Klas Modin - Statistical mechanics, 2-D fluids, and structure preserving numerics
Summary
TLDRThe lecture explores the intricacies of the 2D Euler equations, linking their geometric properties and behavior to symplectic geometry and Hamiltonian systems. The speaker, an experienced professor, shares insights into these mathematical frameworks, highlighting their significance in understanding fluid dynamics on two-dimensional surfaces. The lecture also addresses the challenges associated with numerical simulations, which often fail to preserve essential geometric structures and long-term behavior. The speaker discusses innovative approaches, such as quantization, to create more effective numerical models. This perspective enables a deeper understanding of the underlying conservation laws and dynamics intrinsic to the Euler equations. Overall, the talk underscores the beauty and complexity of these equations, detailing mathematical contributions and the development of symplectic numerical methods that potentially offer more accurate approximations and solutions.
Takeaways
- 🎓 The speaker has a rich academic background, having worked at multiple universities.
- 🔍 The 2D Euler equations are central to the discussion, relevant in fluid dynamics modeling.
- 🥇 Symplectic geometry plays a significant role in understanding these equations.
- 💡 Geometric conservation laws are crucial for the Euler equations' structure.
- 🖥️ Quantization offers innovative numerical approaches to approximate these equations.
- 🎯 Numerical simulations need to preserve the equations' inherent geometry for accuracy.
- 🔄 Traditional numerical methods may not capture long-term behavior effectively.
- 📊 Matrix methods are proposed to enhance understanding and simulation accuracy.
- 🌊 Vorticity and vector fields are key concepts in the Euler equations analysis.
- ↔️ Hamiltonian systems provide a framework for exploring dynamical equations.
Timeline
- 00:00:00 - 00:05:00
The speaker begins by summarizing the academic and professional journey of a colleague named 'Sotru' who has received recognition for his contributions, particularly in preserving geometrical structures in mathematical developments. The speaker is also preparing to discuss their interest in the 2D Euler equations and their geometrical implications.
- 00:05:00 - 00:10:00
The speaker acknowledges the introduction and mentions being in Pisa for the second time. They recall having a related discussion about the Euler equations and their geometric beauty, specifically focusing on the 2D Euler equations' formulation on two-dimensional surfaces and manifold structures.
- 00:10:00 - 00:15:00
Euler's perspective on pressure and how it relates to vector fields being divergence-free is discussed. The speaker explains how the Euler equations connect with Newton's equations and highlights the Helmholtz decomposition in achieving incompressibility within fluids.
- 00:15:00 - 00:20:00
The speaker explains the Euler equations' geometric aspects, having researched related equations in shape analysis. They emphasize the vorticity function, derived using curl, to understand the equations better. The description includes how the vorticity is transported by velocity fields related to Hamiltonian functions, a stream function's geometric interpretation, and the 2D Euler equations' unique structure.
- 00:20:00 - 00:25:00
The speaker discusses the long-term behavior of 2D Euler equations, acknowledging their global solutions, unlike 3D Euler equations. Statistical mechanics and their application to 2D Euler equations are mentioned, along with historical references to using these equations to understand phenomena like planetary storms.
- 00:25:00 - 00:30:00
The speaker describes three approaches to studying 2D Euler equations: statistical mechanics by Onsager, numerical simulations, and rigorous PDE analysis. They highlight challenges in proving longtime behavior with PDE analysis and introduce numerical solutions that might approximate dynamics closely.
- 00:30:00 - 00:35:00
The speaker highlights how, unlike traditional numerics, structure-preserving numerical methods are crucial for capturing qualitative longtime behavior. While traditional methods focus on tracking single trajectories, newer approaches incorporate conservation laws and phase flow properties for more accurate analysis.
- 00:35:00 - 00:40:00
To understand the geometrical properties, the speaker introduces the concept of using Lie groups and invariant Hamiltonian systems. This includes introducing the configuration space as a Lie group and discussing how the dynamics on this space illustrate certain geometrical structures, which relate to 2D Euler equations.
- 00:40:00 - 00:45:00
The speaker explains how vorticity and the concept of point vortices arise from the symplectic structure of fluids, Newtonian mechanics, and Hamiltonian formulations. They discuss how the 2D Euler equations reflect dynamics on coadjoint orbits, with a focus on Casimir functions and how they maintain certain properties during flow.
- 00:45:00 - 00:51:24
Discussing quantization of Euler equations, the speaker outlines Vladimir Zeitlin's approach from 1991, which involves approximating the symplectic structure via finite-dimensional operators. They explain how this framework allows for statistical mechanics interpretations and potentially helps in discretized numerical applications.
Mind Map
Video Q&A
What is the main focus of the lecture?
The lecture focuses on the 2D Euler equations, symplectic geometry, Hamiltonian systems, and numerical simulations.
Who is the speaker, and where have they worked?
The speaker has worked at various universities and joined Charmers in 2013 as a full professor.
What is the Euler equation in 2D?
The 2D Euler equations describe a vector field that is time-dependent, primarily used to model fluid dynamics on a two-dimensional surface.
Why are the geometric properties of the Euler equations significant?
The geometric properties highlight the underlying structure, leading to a better understanding of the equations and the preservation of certain conservation laws.
What is a Hamiltonian system?
A Hamiltonian system is a type of dynamical system governed by Hamilton's equations, which are based on a function called the Hamiltonian.
What practical application does the speaker discuss regarding numerical simulations?
The speaker discusses using numerical simulations to understand the longtime behavior of 2D Euler equations.
How does quantization relate to Euler equations?
Quantization is used to approximate symplectic structures and provides a way to understand the Euler equations in terms of matrix approximations.
What are some challenges the lecture mentions in using traditional numerical methods?
Traditional numerical methods struggle with preserving the geometry and conservation laws inherent in the Euler equations, especially for long-time behavior.
What does the speaker propose for improving numerical methods?
The speaker suggests preserving symplectic structures in numerical simulations to better understand qualitative long-term behavior of Euler equations.
How does the speaker describe the complexity of analyzing Euler equations?
The speaker describes it as complex, noting that true mixing in a smooth sense cannot happen due to the transportation of level sets.
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- 00:00:16today let me just remind we are planning
- 00:00:19to do
- 00:00:20this mon
- 00:00:22or we
- 00:00:29[Music]
- 00:00:47sotru
- 00:00:50here from
- 00:00:53University
- 00:00:54so 2010 at University and then at
- 00:01:00experience at n
- 00:01:02University and University of Canada and
- 00:01:06then in 2013 he joined Charmers where
- 00:01:10got full profess
- 00:01:14in
- 00:01:17so severals and words
- 00:01:22mention from European
- 00:01:25and
- 00:01:28as by
- 00:01:32also
- 00:01:34also
- 00:01:39start so concerning mathematical
- 00:01:41contribution one this major contribution
- 00:01:44is development
- 00:01:49Camp
- 00:01:52IM which preserve
- 00:01:56certain geometrical
- 00:01:58structure anyway
- 00:02:06this is
- 00:02:09particular Sy for long to
- 00:02:13investigate
- 00:02:15long
- 00:02:19Sy and here from here you see see
- 00:02:23thatch is quite a lot of that among
- 00:02:27different FS uh of course
- 00:02:32geometry
- 00:02:43[Music]
- 00:02:52also okay thank you very much can you
- 00:02:54hear me well yes okay
- 00:02:57good thanks a lot for that very very
- 00:03:00nice introduction and thanks for
- 00:03:01inviting me here it's my second time in
- 00:03:04Piza last time was not that long ago
- 00:03:06about half a
- 00:03:08year and then I also got gave a a
- 00:03:12presentation
- 00:03:13um about related a related topic uh so
- 00:03:18there will be probably some overlap but
- 00:03:20I hope not too much in fact uh yesterday
- 00:03:24during
- 00:03:25lunch we had a very nice lunch and then
- 00:03:28Dario said okay okay so it was a nice
- 00:03:31talk you gave last time but maybe you
- 00:03:33can say something more about this
- 00:03:36quantization business which is related
- 00:03:39to the numerical methods that we're
- 00:03:42using and then uh he shouldn't have said
- 00:03:44that because because because then I got
- 00:03:48all excited about what I think is the
- 00:03:50most beautiful part of um of the oiler
- 00:03:53equations namely their the rich geometry
- 00:03:57okay and um so I will tell you a little
- 00:04:00bit about this and then try to connect
- 00:04:03it uh to to various Fields as uh as
- 00:04:06Mario was
- 00:04:08saying so um we are I'm interested in
- 00:04:12right today I'm interested in the 2D uh
- 00:04:15Oiler
- 00:04:15equations so so here you see uh a
- 00:04:19formulation of the two de Oiler
- 00:04:21equations more or less as Oiler wrote
- 00:04:24them down in 1757 he did it in both two
- 00:04:28and three dimensions
- 00:04:30um so the only thing that is slightly
- 00:04:33different here is that we we do it
- 00:04:35generically on on any two-dimensional
- 00:04:37surface I call that surface M so that
- 00:04:40has a manifold
- 00:04:41structure and also with a remanion
- 00:04:43structure on
- 00:04:45it um so so these are the equations and
- 00:04:48and the equations kind of describe a a
- 00:04:51vector field that is time dependent and
- 00:04:55this Vector field describes how the
- 00:04:56fluid is moving the velocity field of
- 00:04:59the
- 00:05:00fluid okay so probably most of you have
- 00:05:04seen this before there is also this
- 00:05:06mysterious it's actually not so
- 00:05:08mysterious this pressure here pressure
- 00:05:10is a function the physicists have their
- 00:05:13point of view but actually if you read
- 00:05:16the original paper by by Oiler you see
- 00:05:18that his view on this is exactly the
- 00:05:20same view that many mathematicians have
- 00:05:24namely that this comes from a projection
- 00:05:26this is due to the fact that when you
- 00:05:28look at these Oilers equations and they
- 00:05:30they Oiler derive them from Newton's
- 00:05:33equations so if you if you look at this
- 00:05:36term here that is not going to be
- 00:05:38Divergence free and we want the vector
- 00:05:40field to be Divergence free because we
- 00:05:42assume that our fluids is
- 00:05:43incompressible okay so you want the the
- 00:05:46the the the vector field to remain
- 00:05:48Divergence free but this one qu of
- 00:05:50points outside the space of Divergence
- 00:05:54re Vector Fields so you need to
- 00:05:55compensate for that and what Oiler
- 00:05:58realized that the optim way to
- 00:06:00compensate namely kind of the orthogonal
- 00:06:02to to this subset of vector fields we
- 00:06:05given by the
- 00:06:06gradients so today we just refer to the
- 00:06:09helm hols decomposition but Oiler
- 00:06:12figured this out long before Helm hols
- 00:06:14was even born it's quite
- 00:06:16impressive okay so so so that's where
- 00:06:19the how we think of the pressure and
- 00:06:20these are the equations so I said I you
- 00:06:24know these Oiler equations they have a
- 00:06:26lot of kind of geometry attached to them
- 00:06:29and I will try to say something about
- 00:06:31this geometry in fact that for many many
- 00:06:34years understanding that geometry was uh
- 00:06:38my field of research um that's where the
- 00:06:43first postto I did in New Zealand was
- 00:06:45about understanding that not for fluid
- 00:06:47equations but for kind of related
- 00:06:49equations that shows up in shape
- 00:06:51analysis and various Fields so I was not
- 00:06:53so interested in fluids but then um I
- 00:06:57had a student
- 00:07:00milu Vivani uh and we we found some
- 00:07:04interesting numerical problem related to
- 00:07:06the two de Oiler equations and then I I
- 00:07:09gradually realized that the gem among
- 00:07:12all this class of geometric equations
- 00:07:15that I'm going to express a little bit
- 00:07:16is actually this two dimensional one
- 00:07:18because it's the one that has most of
- 00:07:22the structure in
- 00:07:24fact uh so so let me kind of describe
- 00:07:28that a little bit probably if you have
- 00:07:30studied the two the oiler equations you
- 00:07:32know that when you want to understand
- 00:07:34this equation what you typically do you
- 00:07:36don't think of it in terms of the vector
- 00:07:38field instead you construct what is
- 00:07:40called a verticity function you can do
- 00:07:42this in three dimensions as well only in
- 00:07:44three dimensions it's not a function
- 00:07:46okay but here the verticity is a
- 00:07:49function and kind of you know if if you
- 00:07:53don't want to explain this in terms of
- 00:07:55geometry what you're doing is you just
- 00:07:56take your vector field and you take the
- 00:07:58curl of that Vector field that is your
- 00:08:00vorticity function and then they try to
- 00:08:02express everything just in terms of this
- 00:08:04this function and then you're led to to
- 00:08:07new set of equations which I've write
- 00:08:09like this so the this here is a Pon
- 00:08:13bracket so this stresses actually the
- 00:08:16the underlying geometry that kind of
- 00:08:18pops out here uh but what this means
- 00:08:21really is that the the verticity
- 00:08:24function is
- 00:08:26transported by the the velocity f
- 00:08:30and furthermore the velocity field since
- 00:08:32it is Divergence free that velocity
- 00:08:35field corresponds to a hamiltonian
- 00:08:37function on this two-dimensional
- 00:08:39manifold that hamiltonian function we
- 00:08:41call the stream function okay so here is
- 00:08:44the geometric interpretation you you
- 00:08:46take you take uh the level sets of this
- 00:08:49stream function which is related to the
- 00:08:52to the vorticity via the the laas
- 00:08:54operator Quon
- 00:08:56equation and then uh you look at the
- 00:08:59gradient of the stream function and you
- 00:09:01just rotate it it's called The skew
- 00:09:02gradient and this in fact corresponds to
- 00:09:05the the hamiltonian vector field for the
- 00:09:08stream function as a hiltonium function
- 00:09:11okay but it's but we don't fix the
- 00:09:13stream function it's it evolves in time
- 00:09:16so it's not like we're just integrating
- 00:09:18one vector field the stream function is
- 00:09:20part of the
- 00:09:21Dynamics so so then you get this
- 00:09:23vorticity formulation of the oil
- 00:09:25equations and just by looking at this
- 00:09:28you get a lot you see a lot of
- 00:09:30structure and
- 00:09:33uh I mean why are the 2 de equations uh
- 00:09:38interesting well for several reasons
- 00:09:41mathematically I suppose it's
- 00:09:43interesting because they
- 00:09:45are let's say easy enough that we can
- 00:09:49prove that there are Global Solutions
- 00:09:51Global in time solutions to these
- 00:09:54equations
- 00:09:56okay so so that's nice this some
- 00:09:59analysis that shows us that solution
- 00:10:01exists for all time you know that we we
- 00:10:04don't know if this true and it's
- 00:10:05probably not true for the 3D
- 00:10:07equations you know that's a different
- 00:10:09story but for 2D we know that it's true
- 00:10:13okay yovich did this already in the 60s
- 00:10:15I think
- 00:10:18so uh so so once you have that you can
- 00:10:22ask okay so what is going on then if if
- 00:10:25you look at kind of is there some sort
- 00:10:27of asymptotic behavior what happens when
- 00:10:30you run when you you run these equations
- 00:10:33for very long is there some kind of
- 00:10:36asymptotic behavior that you can can
- 00:10:38look at and initially you would say uh
- 00:10:41probably not because
- 00:10:45uh you know why should there be it's a
- 00:10:47hamiltonian system hamiltonian systems
- 00:10:50are not like gradient flows that kind of
- 00:10:52converge to something so we don't expect
- 00:10:55them to converge to something right in
- 00:10:58fact they will not converge to something
- 00:11:00I will talk more about this but still
- 00:11:02there is something you can say about the
- 00:11:03longtime
- 00:11:04Behavior okay and this story to try to
- 00:11:09understand the longtime Behavior well in
- 00:11:12some sense it started already by the
- 00:11:14time that people understood that there
- 00:11:16are storms right because if you take as
- 00:11:19a simple approximation of the atmosphere
- 00:11:21just the two de Oiler equations then
- 00:11:23eventually you see these storms forming
- 00:11:25and it seems to be that they are quite
- 00:11:27stable not completely stable but quite
- 00:11:30stable if you look at other planets like
- 00:11:32Jupiter for example then you see very
- 00:11:35big storms that are very stable like the
- 00:11:38Red Spot on Jupiter is actually a big
- 00:11:40storm so you can ask what makes these
- 00:11:43kind of
- 00:11:44formations stable why why do they
- 00:11:50appear and so that's a very natural
- 00:11:54question and there are different
- 00:11:56approaches for studying this problem
- 00:11:58studying the long time behavior of these
- 00:12:00two de oil equations and what I would
- 00:12:02say one of the gems in the field is to
- 00:12:06make progress on this problem okay so I
- 00:12:10I I've listed here the the three
- 00:12:12approaches that I consider there might
- 00:12:13be others but I consider these like the
- 00:12:15the main approaches and this
- 00:12:18goes uh you know this covers both
- 00:12:21physics and
- 00:12:23Mathematics so the first approach I I
- 00:12:25mean maybe I should not list it at this
- 00:12:28first but this one approach which the
- 00:12:29physicist like very much is to apply
- 00:12:33statistical mechanics to the problem so
- 00:12:36the first one to do this to apply
- 00:12:38statistical mechanics to the two de
- 00:12:39Oiler equations was l uner in 1949 he
- 00:12:43wrote one paper about this which became
- 00:12:46a legendary paper in fluid dynamics only
- 00:12:48one paper uh but it has led to a a big
- 00:12:52field of both mathematics and physics
- 00:12:54that that paper Al but what is
- 00:12:57statistical mechanics when you think
- 00:12:59about it well it's something you take
- 00:13:01some dynamical system and you try to
- 00:13:05understand what I mean Bas it's like
- 00:13:09probability applied to uh to dynamical
- 00:13:13systems hamiltonian
- 00:13:15systems so and you try to understand
- 00:13:18where in phas base is it most common to
- 00:13:21be you know where where does most States
- 00:13:24wants to be in face space so this is the
- 00:13:26underlying idea if you like of
- 00:13:28statistical mechanics that the boltzman
- 00:13:31uh was developing for gas Dynamics but
- 00:13:34unog's brilliant idea was to apply this
- 00:13:37to the fluids I will tell you more about
- 00:13:38exactly
- 00:13:39how um but the interesting thing here is
- 00:13:42that what do you use from the actual
- 00:13:44Dynamics the dynamical system that you
- 00:13:46start with which in this case is
- 00:13:48infinite dimensional what do you
- 00:13:50actually use so you use that um there is
- 00:13:54a
- 00:13:55leoville structure to the equations
- 00:13:57namely that pH BAS volume is
- 00:14:00preserved so for hamiltonian systems
- 00:14:02that's automatic because it follows from
- 00:14:04the fact that the flow is simplec so you
- 00:14:07always have this Lille property and
- 00:14:09that's very
- 00:14:10important H the other thing you use from
- 00:14:12the Dynamics is that there are
- 00:14:13conservation laws typically at least
- 00:14:16energy could be others as
- 00:14:19well but the rest of the Dynamics you
- 00:14:21kind of throw away and then you just say
- 00:14:24uh assuming that I know these kind of
- 00:14:26macroscopic variables and I put them as
- 00:14:29constraint and then I make the
- 00:14:30assumption that all the states
- 00:14:34microscopic States corresponding to this
- 00:14:37uh microscopic state have the same
- 00:14:40probability more or less this is the
- 00:14:42intuition behind statistical mechanics
- 00:14:45okay so you throw away a lot of the
- 00:14:47Dynamics and just see okay what if I
- 00:14:50make these assumptions and by the way
- 00:14:52this is connected to the assumption that
- 00:14:54the flow is erotic it's very much
- 00:14:56connected to this so you make this
- 00:14:58assumption and then normally you need to
- 00:15:01make some sort of discretization as well
- 00:15:03at least if this system is initially
- 00:15:05infinite dimensional
- 00:15:08because you know otherwise uh it doesn't
- 00:15:12statistical mechanics essentially
- 00:15:13doesn't make sense you need to to
- 00:15:15truncate it somehow make it finite
- 00:15:17dimensional so there's some
- 00:15:18discretization involved also here but
- 00:15:20not discretization to kind of of the
- 00:15:23Dynamics but rather of the face bace
- 00:15:26somehow
- 00:15:30um so and then this gives you
- 00:15:32predictions about what will happen or
- 00:15:34what is most common so and then and then
- 00:15:37the saying is if you're in a place in
- 00:15:39face base which is not so common and
- 00:15:41probably most of the time it will kind
- 00:15:43of move towards some other part of face
- 00:15:45base which is more
- 00:15:47common okay that's a neat idea and then
- 00:15:51you work surprisingly well actually so
- 00:15:55the other approach is to to carry out
- 00:15:57numerical simulations
- 00:15:59so this is uh another approach where you
- 00:16:04the it comes in two flavors I will say
- 00:16:06something about this but normally what
- 00:16:08you do you start with the equations and
- 00:16:10then you discretize them in space and in
- 00:16:13time you end up with some new Dynamics
- 00:16:17which you now can actually Implement as
- 00:16:19an algorithm in the computer you solve
- 00:16:21for this and then you hope that whatever
- 00:16:24discretizations you used will
- 00:16:26approximate the flow good enough so that
- 00:16:30somehow it corresponds to the the the
- 00:16:33true dynamics that you're interested in
- 00:16:35and then if you're if you're a good uh
- 00:16:37numerical analyst you will not only make
- 00:16:40the discretization you will also prove
- 00:16:43that as I made the discretization better
- 00:16:45and better this will actually converge
- 00:16:47to the true solution of the of the
- 00:16:49equations this is the traditional
- 00:16:51numerical approach to to PDS let's
- 00:16:55say and then of course uh the other
- 00:16:58branch
- 00:16:59uh which is probably you know the most
- 00:17:02mathematical one and for some people
- 00:17:04it's the only one is that you you apply
- 00:17:07as much analysis in PD geometric
- 00:17:10analysis you can to these equations to
- 00:17:12try to understand the solutions okay so
- 00:17:15this is uh here you you you really look
- 00:17:18at the exact Dynamics you you try to
- 00:17:21prove rigorous results but it's usually
- 00:17:24very hard okay we can Pro we can prove
- 00:17:27things like Global existence but to say
- 00:17:29something about the longtime Behavior
- 00:17:32rigorously with PD analysis is a very
- 00:17:35very hard
- 00:17:36problem okay so normally what you can
- 00:17:39say the the state-ofthe-art today for
- 00:17:41this kind of approach is that you start
- 00:17:44with some uh near steady state solution
- 00:17:48and then you maybe say that it will
- 00:17:50remain near steady state for for that's
- 00:17:53the kind of predictions you can get with
- 00:17:54this this is like perturbations of
- 00:17:57things that we we fully understand
- 00:18:01so so in a way I I put numerics here in
- 00:18:04the middle because I think of it as
- 00:18:07something in
- 00:18:09between this and this right so let me
- 00:18:12explain why
- 00:18:16so in numerics you take some concern to
- 00:18:20the Dynamics your approximate the
- 00:18:23Dynamics okay so you you do care about
- 00:18:25the the Dynamics but if you do the
- 00:18:27numerics carefully not everyone is doing
- 00:18:30that but if you do it carefully and
- 00:18:31you're you're interested in longtime
- 00:18:32Behavior you should also care about
- 00:18:35these other things that that that you do
- 00:18:39that are important in statistical
- 00:18:42hydrodynamics for example that the phase
- 00:18:44flow is is preserves deliv property is
- 00:18:48volume preserving and also that you have
- 00:18:51conservation laws okay so you should try
- 00:18:53to replicate those in your
- 00:18:56discretizations and this is kind of
- 00:18:59what separates what I what what I will
- 00:19:02call Matrix hydrodynamics applied to
- 00:19:05this uh equation from traditional
- 00:19:07numerics where you traditional numerics
- 00:19:09you essentially try to follow a single
- 00:19:11trajectory as well as you can and
- 00:19:15sometimes that's what you want you want
- 00:19:16to follow a single trajectory as well as
- 00:19:19you can to uh understand what is
- 00:19:22happening for that single trajectory but
- 00:19:24that's not really the problem we're
- 00:19:25interested in here we're interested in
- 00:19:27the qualitative long time Behavior okay
- 00:19:30and for the oiler equations if you
- 00:19:32follow a single trajectory even if you
- 00:19:34do that extremely well eventually they
- 00:19:37will diverge from the true solution
- 00:19:39because uh because it's a kind of a
- 00:19:42chaotic system it's very very sensitive
- 00:19:44for perturbations of your initial
- 00:19:47data so that's why I claim that
- 00:19:50traditional numerics is good for
- 00:19:52shorttime trajectory tracking but it's
- 00:19:55not good for long time qualitative
- 00:19:57Behavior then you really need to involve
- 00:20:00some of the structure that we know is
- 00:20:02important from statistical mechanics
- 00:20:04namely all the conservation laws and
- 00:20:05their phase flow
- 00:20:07property okay so that was uh kind of a
- 00:20:10long
- 00:20:11introduction um so now I said that it's
- 00:20:14important to preserve all this geometry
- 00:20:16let me say something about more about
- 00:20:19this geometry what it what it actually
- 00:20:21comes from and I will do it first in a
- 00:20:24kind of abstract way and U if you
- 00:20:27haven't seen this before it might be uh
- 00:20:31a bit much but relax because I will
- 00:20:34connect it to the oiler equations the
- 00:20:37two de Oiler equations so that you see
- 00:20:39what's what's going on in fact I'm
- 00:20:41essentially only interested in two the
- 00:20:43oiler equations on the two
- 00:20:45sphere
- 00:20:47okay so here is the kind of abstract
- 00:20:50framework you start with some
- 00:20:51configuration space which is not like
- 00:20:54particles in space but rather consists
- 00:20:57of a Le group so so there's a group
- 00:20:59structure to your configuration and then
- 00:21:02you look at hamiltonian system for that
- 00:21:04configuration space that means you have
- 00:21:05some hamiltonian which involves not just
- 00:21:08the configuration variable which is you
- 00:21:10can think of as for example a rotation
- 00:21:12Matrix if it describes a rigid body but
- 00:21:15also some Associated momentum variable
- 00:21:18geometrically this means we look at
- 00:21:19points the face base consists of the
- 00:21:21cotangent ble of this uh of this leag
- 00:21:24group and then to get hamiltonian
- 00:21:27Dynamics what you need you need a
- 00:21:30hamiltonian uh so that's a function of
- 00:21:32the configuration variable q and the
- 00:21:35corresponding momentum variable which is
- 00:21:37kind of the momenta sitting above the
- 00:21:38point think of it as as
- 00:21:40[Music]
- 00:21:42a an configuration and a corresponding
- 00:21:45uh momentum variable or velocity
- 00:21:48variable associated with that but but we
- 00:21:51put some constraints on our D Dynamics
- 00:21:54so we say that in fact because we have
- 00:21:56this group structure we say that our
- 00:21:57hamiltonian is invariant under the
- 00:22:00action of the group
- 00:22:01itself okay so what does this mean think
- 00:22:05of a rigid body rigid body is described
- 00:22:09by I take this pan by by an a matrix an
- 00:22:14orthogonal Matrix with determinant one
- 00:22:17that describes its orientation right so
- 00:22:20that's my all my
- 00:22:21configurations and then I want my
- 00:22:23hamiltonian describing this to be
- 00:22:25invariant under how I kind of rotate the
- 00:22:28object so this has a natural Symmetry
- 00:22:30and a lot of problems in physics
- 00:22:32actually have the Symmetry and the cool
- 00:22:35thing that in fact the fluid also has
- 00:22:37this symmetry you think about it like
- 00:22:39this I'll come to that but the fact that
- 00:22:41you have this symmetry means that in the
- 00:22:44end you can reduce the Dynamics from
- 00:22:46this cotangent bundle in quent out by
- 00:22:49the Symmetry and what you end up with
- 00:22:51and this is if you like this is uh like
- 00:22:55Le
- 00:22:56algebra things but think of it as you
- 00:22:59have some symmetry you reduce out that
- 00:23:01Symmetry and you end up if your
- 00:23:03configuration space is a Le group you
- 00:23:05actually end up in a vector space that
- 00:23:07Vector space is just the Dual of the Le
- 00:23:10algebra of of your your your Le group
- 00:23:15okay I want to kind of go quickly here
- 00:23:18because the point is once you have such
- 00:23:21a system you can abstractly write it as
- 00:23:23some equation just on the Duel of the
- 00:23:26Lee algebra okay this is called the Le s
- 00:23:28system those were the kind of systems
- 00:23:30that I was I was studying long before I
- 00:23:33got interested in fluids but not in
- 00:23:36particular for for the fluid
- 00:23:39okay but such systems also have a
- 00:23:42hamiltonian structure that they kind of
- 00:23:45inherit from the original Honan
- 00:23:47structure it's just that it's not a
- 00:23:49canonical Honan structure it's not the Q
- 00:23:51and P
- 00:23:52variable uh it's it's it's what it's
- 00:23:55called a pon pon structure
- 00:23:59okay but in fact you can still recover
- 00:24:02the Q and P variables somehow because
- 00:24:06every such Pon structure Pon manifold uh
- 00:24:10is kind of foliated
- 00:24:13into sub manifolds in the best case they
- 00:24:15are sub manifolds and these are called
- 00:24:18the simplec leaves and each such sub
- 00:24:21manifold is a simplec manifold and then
- 00:24:23you know the daru theorem that on each
- 00:24:25simplec manifold you can put canonical
- 00:24:27coordinates so locally you can in fact
- 00:24:30reduce this system even more by
- 00:24:32restricting to one of these simplec
- 00:24:34leaves because once you start on one you
- 00:24:36will never leave it okay and this by the
- 00:24:39way for the fluids I'm skipping apart
- 00:24:41has to do with the fact that there are
- 00:24:42infinitely many conservation laws for
- 00:24:44two the oiler equations so the Casimir
- 00:24:46functions it just means that you remain
- 00:24:48on these coant orbits
- 00:24:50okay and formally the coadjoint orbits
- 00:24:53are given you take the the action of the
- 00:24:57group on its algebra and then that
- 00:25:00induces an action on the Dual of the Le
- 00:25:02algebra that's called a coint action we
- 00:25:04write add star this operator here okay
- 00:25:08so the Dynamics will remain on this
- 00:25:10coadjoint orbits that's one of the main
- 00:25:12messages from from this Vos Dynamics so
- 00:25:15let's apply this now to the two de Oiler
- 00:25:17equations what is the
- 00:25:19group okay the group has to be infinite
- 00:25:22dimensional because we know it's a flow
- 00:25:24on some infinite dimensional space the
- 00:25:26beautiful thing and this is due to oural
- 00:25:28is that the group is the space of
- 00:25:31simplecom morphisms or area preserving
- 00:25:34maps of the
- 00:25:36manifolds
- 00:25:38okay uh
- 00:25:40so that's the group write it like this
- 00:25:43diff mu mu is the volume or the area
- 00:25:45form so in this case it's the simplec
- 00:25:48structure on these two dimensional
- 00:25:50manifold just just think of it as the
- 00:25:51area
- 00:25:52form so the Le algebra of a Le group is
- 00:25:56the tangent space at the identity this
- 00:25:58comes out as what Divergence free Vector
- 00:26:01fields which in the two-dimensional case
- 00:26:03corresponds to simplec Vector Fields so
- 00:26:06these are really the the simplec vector
- 00:26:08fields and I put a little star here
- 00:26:11because this is not always true you have
- 00:26:12to assume that they're uh there some
- 00:26:15topological properties of your manifold
- 00:26:17the first cohomology has to be trivial
- 00:26:19if that's true which is true on the
- 00:26:20sphere then every simplec manifold every
- 00:26:23simplec Vector Fields can be written in
- 00:26:25terms of a generator or a hamiltonian
- 00:26:27function that's the one we call the
- 00:26:29stream function in fact so this space of
- 00:26:33hamiltonian vector Fields is
- 00:26:35parameterized by stream function and the
- 00:26:37stream function is unique up to some
- 00:26:40constant so the natural kind of space of
- 00:26:44simple of hamiltonan vector Fields is
- 00:26:47just the smooth functions modul the
- 00:26:52constants okay so I said we wanted to
- 00:26:54work with the Dual so now we need to
- 00:26:56take the Dual of this Beast here here of
- 00:26:58course the Dual of some space of smooth
- 00:27:02functions is a nasty
- 00:27:05object it's a you know you can put if
- 00:27:08you want to put topologies on this basis
- 00:27:11the the if m is compact the natural
- 00:27:13thing is to put the fresh a topology
- 00:27:15here and then the Dual of a fresh a
- 00:27:18space which is not the Bono space not
- 00:27:19even a fresh a space so this is a nasty
- 00:27:22thing okay so what you do is you say
- 00:27:25okay let us restrict restrict ourself a
- 00:27:29little bit just to what is called the
- 00:27:31smooth part of the jewel so you consider
- 00:27:34elements in the jewel so those are are
- 00:27:38one forms like this which are determined
- 00:27:41by some smooth function okay and in
- 00:27:44order for this to actually descend to
- 00:27:46the the quotient here you you you have
- 00:27:48to require that this function integrates
- 00:27:50to zero so it has mean value
- 00:27:53zero this is the how you kind of
- 00:27:55normally do this but I wanted to stress
- 00:27:57it because it's in fact important to
- 00:28:00realize that sometimes you need to move
- 00:28:03to this full
- 00:28:04Jewel why is it okay to restrict to the
- 00:28:07smooth duel well if you remember the
- 00:28:10Dynamics remains on the coadjoint orbits
- 00:28:13and the point is if you start on some
- 00:28:16smooth with on a smooth um verticity it
- 00:28:21will remain smooth if so if you start in
- 00:28:23the smooth duel it will remain smooth
- 00:28:25because you're acting on it with diffuse
- 00:28:27so the actual of of a function the
- 00:28:29action by the way is just by composition
- 00:28:31of the inverse so this is going to
- 00:28:34preserve the smooth structure of the
- 00:28:35function okay so if you start with
- 00:28:38something smooth then and apply a nice
- 00:28:40diffo you remain smooth okay so in that
- 00:28:43sense it's okay to work with just a
- 00:28:44smooth
- 00:28:46duel uh and now you can ask okay so what
- 00:28:51is Theon equation to get the leason
- 00:28:53equation we have to also specify a
- 00:28:55hamiltonian function and the hamiltonian
- 00:28:57function we specify is just this one so
- 00:29:01it's quadratic corresponding to the H
- 00:29:04minus1 Norm on the space of
- 00:29:07functions okay so if you write it in
- 00:29:11terms of the string function is this
- 00:29:12thing here and then you write down the L
- 00:29:14Leon system and out pops exactly the two
- 00:29:18the oiler equations in vorticity form so
- 00:29:20that's the beauty of these equations it
- 00:29:22can be interpreted as some hiltonium
- 00:29:25flow on the cotangent bundle of a space
- 00:29:27of dorph
- 00:29:29a simplec diff morphisms and in fact
- 00:29:33this hamiltonian description describes
- 00:29:35geodesics on the space of diffuse this
- 00:29:38is Arnold's big Discovery from
- 00:29:401966 I don't say so much here but but
- 00:29:43the hamiltonian side is interesting
- 00:29:45enough let's say you can also have a
- 00:29:48Rania side of this so so so this is how
- 00:29:51kind of the geometry pops out see where
- 00:29:53I am in
- 00:29:55time yeah uh
- 00:29:58um and I said something that you know
- 00:30:01there are some a lot of conserved
- 00:30:04properties here and essentially where
- 00:30:06does the from the geometric perspective
- 00:30:08where do these properties come from well
- 00:30:11if you take a function now in this large
- 00:30:13pH base of all vorticity
- 00:30:16functions um and you know you're going
- 00:30:19to remain on the coant orbit so if you
- 00:30:21take any
- 00:30:22function on or any
- 00:30:25functional uh on the space of verticity
- 00:30:31functions that is constant on the coant
- 00:30:33orbits that's going to be preserved by
- 00:30:36the
- 00:30:37flow and these functions are the ones
- 00:30:39called Casmir Casmir
- 00:30:41functions and and here is how you
- 00:30:43construct them uh you just take some
- 00:30:46function from R to R
- 00:30:49okay and then you you just compose this
- 00:30:52function with with your uh your uh your
- 00:30:55smooth verticity field and you integrate
- 00:30:57with respect to your simplec structure
- 00:31:00your area form okay and the proof that
- 00:31:03this is preserved well you see easily by
- 00:31:05a change of variable that this is
- 00:31:07preserved on the coent orbit and because
- 00:31:10we remain on the coent orbit it has to
- 00:31:12be preserved okay so so so these are
- 00:31:15infinitely many custom unit one for each
- 00:31:18function
- 00:31:20f normally you take F to be polinomial
- 00:31:22monomial
- 00:31:24even um
- 00:31:26okay so here is connecting back a bit to
- 00:31:30this full story of the full Jewel which
- 00:31:32was a nasty object so what happens if
- 00:31:35you start on a coint orbit which is not
- 00:31:38a smooth coint
- 00:31:40orbit so maybe I didn't say that but the
- 00:31:46interpretation of this coadjoint orbit
- 00:31:48is that you you kind of look at the
- 00:31:50level sets of your vorticity function
- 00:31:54and and and the action is just moving
- 00:31:56these level sets so the only thing that
- 00:31:58you're allowed to do in the Dynamics is
- 00:32:00to move around the level sets of your
- 00:32:02verticity function that's kind of what
- 00:32:04you're allowed to do that's puts a lot
- 00:32:06of constraints on what you can do right
- 00:32:08and in fact it it kind of explains why
- 00:32:11fluids are so complicated because in
- 00:32:13fluids you sometimes see like vorticity
- 00:32:17Blobs of the same sign that kind of
- 00:32:20undergo some
- 00:32:22mixing but true mixing in the smooth
- 00:32:26sense cannot happen because you're just
- 00:32:29transporting level sets so the only
- 00:32:31thing that happens is that this becomes
- 00:32:32more and more and more intricate and in
- 00:32:35fact it's so intricate that in the end
- 00:32:38if you just take some completion in a
- 00:32:40slightly rougher topology you cannot see
- 00:32:44what has happened okay so this is why
- 00:32:46say at least from my perspective the
- 00:32:48analysis of this equation is is far from
- 00:32:51trivial okay
- 00:32:54um so so you're just transporting levels
- 00:32:56so what happens if you start with some
- 00:32:58verticity that has support just on some
- 00:33:01single on some points you know so you
- 00:33:04start with a Sit situation where the
- 00:33:06verticity is zero everywhere except on a
- 00:33:09few points these points here okay let's
- 00:33:13say four of
- 00:33:15them so so then you can construct the
- 00:33:18corresponding
- 00:33:20uh element in the Dual right this is an
- 00:33:23element in the Dual I just take some
- 00:33:25some strengths here gamma and I and and
- 00:33:28I construct this thing here it's it's
- 00:33:31linear okay so it's an element in the
- 00:33:33Dual um and in fact formally you can
- 00:33:36write this in terms of direct Delta so
- 00:33:39kind of what happens here is that you
- 00:33:41you put you put vorticity it's not mass
- 00:33:44now we put verticity just in a few
- 00:33:48points
- 00:33:49okay and then the point is in the smooth
- 00:33:53setting if I started with a smooth
- 00:33:54vorticity field then it remain Smooth by
- 00:33:56the co induction so what happens if I
- 00:33:59apply the coant action to to this
- 00:34:01strange configuration well it's easy to
- 00:34:04see it's going to uh remain of the same
- 00:34:07form I just moved around these Delta
- 00:34:10pulses okay with my diff
- 00:34:13morphis so in fact it also means that I
- 00:34:15have these finite dimensional coagent
- 00:34:17orbits because I start with finitely
- 00:34:19many let's say n of these direct deltas
- 00:34:23and I'm just moving them
- 00:34:25around okay and it's clear that the ACT
- 00:34:28on these is transitive by the diffuse
- 00:34:30you can move the points to any where you
- 00:34:33like except maybe I so I should take
- 00:34:35away the diagonal here sorry that's a
- 00:34:37mistake because you cannot take two
- 00:34:40points
- 00:34:41and put them on top of each other
- 00:34:43because then you you're no longer a diff
- 00:34:45morphis okay so that cannot happen so I
- 00:34:47should take out the diagonal here but if
- 00:34:49I do that it's a kind of transitive
- 00:34:50action on that on that manifold and that
- 00:34:54manifold is now finite dimensional so I
- 00:34:55have finite dimensional coordinate
- 00:34:57orbits and then I can describe the
- 00:34:59Dynamics on these finite dimensional
- 00:35:00spaces and what comes
- 00:35:03out is point vertices okay so the
- 00:35:07correct geometric interpretation of the
- 00:35:10point Vortex solutions to the oiler
- 00:35:12equations which were found by the way
- 00:35:15long
- 00:35:16before uh this geometry was discovered
- 00:35:19so and it's kind of natural as soon as
- 00:35:21you realize that verticity is being
- 00:35:23transported it's natural to say what
- 00:35:25happens if I transport just a few sing
- 00:35:27points but this is kind of the geometric
- 00:35:30description that these Point vertices
- 00:35:32just correspond to finite dimensional
- 00:35:34coint
- 00:35:35orbits okay of the fluids so now what
- 00:35:40was unog's idea his idea was okay we
- 00:35:44have these two deiler equations I want
- 00:35:46to do statistical mechanics to try to
- 00:35:48predict what happens see if I can see
- 00:35:49these storms forming okay uh but how do
- 00:35:54I do this on an infinite dimensional
- 00:35:56face space doesn't make makes sense it
- 00:35:58needs to be finite dimensional in fact
- 00:36:00it kind of needs to be
- 00:36:02compact so his idea was let's take Point
- 00:36:07vortices instead and restrict them to
- 00:36:09some manifold which is
- 00:36:12compact uh so he he used I think the the
- 00:36:15flat two tourus the dou periodic
- 00:36:18square and he put N Point veses there
- 00:36:21then he gets a finite dimensional
- 00:36:23hamiltonian
- 00:36:25system H and then he said this is a
- 00:36:28realm where I can apply statistical
- 00:36:31mechanics to this finite dimensional
- 00:36:33hamiltonian system and he did that and
- 00:36:38out came This brilliant
- 00:36:40interpretation at uh I think I talked
- 00:36:43about this last time I was here I I
- 00:36:45don't want to spend too much time on it
- 00:36:46but one of oner's great ideas was that
- 00:36:50or what he realized is that even if you
- 00:36:52don't restrict to a specific energy
- 00:36:55level um the the
- 00:36:58energy
- 00:37:00uh uh the the pH base volume is is is
- 00:37:04finite let's say one okay H and because
- 00:37:08of that you see that the the this
- 00:37:11thermodynamical temperature or the
- 00:37:13statistical temperature can be both
- 00:37:15positive and negative and when it is
- 00:37:19negative which cannot happen for a gas
- 00:37:21but it can happen for for this system
- 00:37:23when it's negative then you kind of
- 00:37:25expect that uh uh clusters of Point
- 00:37:30vortices with the same sign will come
- 00:37:34together because that's what the
- 00:37:36statistical mechanics then
- 00:37:38predicts so that was his insight and
- 00:37:40that kind of explains why you see this
- 00:37:42merging of storms right that that
- 00:37:45behavior happening he also realized uner
- 00:37:48himself that that this uh model has it
- 00:37:53its
- 00:37:53weaknesses it's based on point vortices
- 00:37:56typically he said
- 00:37:58say
- 00:38:00uh distributions of vorticity which
- 00:38:03occurs occur in the actual flow of
- 00:38:05normal liquids are continuous of course
- 00:38:08they very far from continuous when
- 00:38:10you're approximating by uh by direct
- 00:38:13deltas and then he says and then he
- 00:38:16realized and here he's saying without
- 00:38:18saying it explicitly for me what he's
- 00:38:20saying is in the continuous case the
- 00:38:22coadjoint orbits look very different
- 00:38:24from in the point Vortex case he saying
- 00:38:27that uh so that convective processes can
- 00:38:31build V vortices only in the sense of
- 00:38:33bringing together volume elements of
- 00:38:35great initial vorticity what he's saying
- 00:38:37is we're just transporting around the
- 00:38:39level sets of vity so not everything can
- 00:38:42be
- 00:38:43reached okay and for me this is just
- 00:38:46means soer kind of realized
- 00:38:48that constraining yourself to staying on
- 00:38:52these coadjoint orbits is is important
- 00:38:55and the coint orbits in the point Vortex
- 00:38:56model are very very different from the
- 00:38:58continuous or smooth quadrant
- 00:39:02orbits so okay so then you can ask this
- 00:39:05is a nice idea of one Sager to take a
- 00:39:07fluid approximate it by Point vortices
- 00:39:11and apply statistical mechanics you can
- 00:39:12also use this to discretize the equation
- 00:39:14think of this as a numerical method
- 00:39:16because in the end you have a finite
- 00:39:17dimensional homoni system you can apply
- 00:39:19some numerical integration scheme to
- 00:39:21this and see what
- 00:39:23happens but still there is this problem
- 00:39:26that unar himself lifted so the question
- 00:39:29is is there another model another finite
- 00:39:32dimensional model of the oiler equations
- 00:39:35where you have all this nice structure
- 00:39:38which kind of fits into this
- 00:39:42framework but still have the something
- 00:39:46corresponding to smooth coant
- 00:39:48orbits okay or or smooth verticity
- 00:39:52fields and the answer is
- 00:39:55yes if you relax a little bit the what
- 00:39:58you mean so you we're not now not no
- 00:40:01longer looking for Exact Solutions we're
- 00:40:03modifying structures a little bit we're
- 00:40:06approximating the structures and this is
- 00:40:08an idea that goes back to Vladimir zlin
- 00:40:11from 1991 and his idea was to take this
- 00:40:15infinite dimensional Bon system and he
- 00:40:18just looked at it well I imagine that he
- 00:40:21just looked at it looked at the
- 00:40:22verticity formulations formulation of
- 00:40:25this system and he said what what do I
- 00:40:27need I need the pon brackets and I need
- 00:40:31a
- 00:40:31lashan how can I approximate a Pon
- 00:40:34bracket and a lashan that's what
- 00:40:37quantization is doing for you okay the
- 00:40:40field that was uh invented by Paul Dr
- 00:40:44that was his idea you know you you you
- 00:40:47you take a Pon algebra of smooth
- 00:40:51functions and you replace it with
- 00:40:53operators in such a
- 00:40:55way that the the Pome bracket is
- 00:40:59approximated by The Matrix
- 00:41:01commutation and and it's not there's no
- 00:41:04exact equality here essentially cannot
- 00:41:06get exact quantization it it it cannot
- 00:41:09happen Okay so you always get an
- 00:41:10approximation here and and then you have
- 00:41:13this H bar also which kind of has to do
- 00:41:16with when this approximation breaks down
- 00:41:19completely if you
- 00:41:21like and so so in our case or what what
- 00:41:25zlin did here was he was thinking about
- 00:41:29taking a verticity field applying to
- 00:41:32quantization to replace this Vector
- 00:41:35field by a matrix because he also knew
- 00:41:39something about quantization Theory and
- 00:41:41he knew that if your underlying manifold
- 00:41:43m is compact there is some chance that
- 00:41:46these operators can be finite
- 00:41:47dimensional so they can be
- 00:41:49matrices okay and this going to be
- 00:41:51because it's quantum mechanics going to
- 00:41:53be a skew herian Matrix actually in
- 00:41:56quantum mechanics you work with herian
- 00:41:57matrices but it's just a matter of
- 00:41:59multiplying with I everywhere so from
- 00:42:01the Le algebraic perspective it's more
- 00:42:04natural to think about SK Herm missan
- 00:42:07Matrix so this is uh the approach and
- 00:42:09this H bar in this case corresponds to
- 00:42:11the size of the Matrix which numerically
- 00:42:14makes perfect sense you have a very
- 00:42:15large Matrix meaning many degrees of
- 00:42:18freedom you can resolve more meaning you
- 00:42:20have a smaller H bar in fact H bar
- 00:42:22scales like one over n where n is the
- 00:42:24size of the Matrix we're looking at n *
- 00:42:26n Matrix skewer Mission
- 00:42:29matrices okay so this is this is the
- 00:42:32idea and the only problem is how do you
- 00:42:34actually do this because we want to in
- 00:42:36the end get something which we can work
- 00:42:38with and Implement in the computer and
- 00:42:40so on so you need explicit schemes for
- 00:42:42how to quantize things and there are
- 00:42:45such schemes um and the ones that sain
- 00:42:48used were developed by Jen Hopper just a
- 00:42:50few years
- 00:42:52earlier um and he was doing it on on on
- 00:42:55various manifolds so in particular this
- 00:42:57flat Taurus and also on S2 I think zlin
- 00:43:00initially did this just on the
- 00:43:03Taurus um but I will be more interested
- 00:43:06in doing this on the sphere in fact and
- 00:43:08this is I this exactly how this works is
- 00:43:11interesting uh and you know every
- 00:43:15mathematician at some point you have to
- 00:43:16study some representation Theory uh and
- 00:43:19I probably did as a student but I didn't
- 00:43:22quite get the points uh but now I
- 00:43:25realize why representation Theory is
- 00:43:27very very important uh because you see
- 00:43:30in this quantization how it kind of pops
- 00:43:32out and it's the it's a it's a very
- 00:43:35natural way to describe this whole
- 00:43:36process so I'm not going to go through
- 00:43:38that because it will take too long but
- 00:43:40essentially this is how it works if you
- 00:43:42think about you know algorithmically how
- 00:43:45you construct these matrices you start
- 00:43:47with some function you expand it in
- 00:43:49spherical
- 00:43:50harmonics and then what the quantization
- 00:43:53gives you is some approximation of these
- 00:43:55spherical harmonics and B matrices and
- 00:43:58the way you you you construct this is it
- 00:44:01comes directly out from from
- 00:44:03representation Theory so you start with
- 00:44:05some symmetry which is in this case is
- 00:44:06the the S SO3 Symmetry and from and then
- 00:44:09you look at all the irreducible
- 00:44:11representations and that you know we
- 00:44:13know there are connections to spherical
- 00:44:15harmonics and then this is how you
- 00:44:17construct these matrices and out from
- 00:44:20this you also get a
- 00:44:22laian which is called the H HOA laian
- 00:44:26which then approximates the the the llin
- 00:44:29on the sphere okay so here is the the
- 00:44:32idea of these Zin equations you take
- 00:44:35your verticity state which is you know
- 00:44:39the variable in your equation you
- 00:44:41quantize it you get a corresponding
- 00:44:44verticity
- 00:44:45Matrix and then what else do you need
- 00:44:48well you need a laian and if you
- 00:44:49quantize that and H Yao tells us that we
- 00:44:52get this H Yao laian which again you can
- 00:44:57explicitly write down uh the formula
- 00:45:00for and uh and then once we have this we
- 00:45:04know what to do because this is how the
- 00:45:05equations look like and now we know that
- 00:45:08the pon bracket is just replaced by the
- 00:45:10commutator so then we get the Matrix
- 00:45:11flow just like this okay and then we can
- 00:45:15once we solve this we can go back and
- 00:45:18ask uh you know uh and interpret this as
- 00:45:22a solution or some approximation to the
- 00:45:25oiler equations what is the benefit of
- 00:45:27this
- 00:45:27approach well first of all what's the
- 00:45:30bad thing with this approach if you if
- 00:45:32you're a numerical analyst typical
- 00:45:35questions you ask are like how well is
- 00:45:39this uh discretization converging when
- 00:45:43the number of degrees of freedom
- 00:45:44increases okay and the other question
- 00:45:47you ask is Convergence how fast does
- 00:45:51Solutions converge assuming that they
- 00:45:52you know if they do converge at
- 00:45:55all uh so so this as an as a kind of
- 00:45:59numerical scheme to approximate smooth
- 00:46:02functions this has very bad order the
- 00:46:06order is like one half because the error
- 00:46:10goes down the discretization error and
- 00:46:12this comes from quation Theory goes down
- 00:46:15like one over n but the number of
- 00:46:17degrees of freedoms is n
- 00:46:20SAR so it's like an one half order
- 00:46:24spatial discretization okay so that
- 00:46:26that's kind of bad for a method right I
- 00:46:28mean if you come say ha look I have a
- 00:46:31numerical method the order the conver
- 00:46:33the convergence order is one half it's
- 00:46:35not so impressive okay so that you have
- 00:46:37to live with because there is an
- 00:46:40something that you gain from this also
- 00:46:41which is that you preserve all this
- 00:46:43richly plusone structure it's all there
- 00:46:46so you have the analog you have coint
- 00:46:48orbits you have all this casmere
- 00:46:51functions or approximations of the
- 00:46:53Casmir functions just contained in this
- 00:46:55framework which is beautiful because
- 00:46:58that means that we have the things or at
- 00:47:01least some approximation of the
- 00:47:02structure that we needed uh in order to
- 00:47:05for statistical mechanics to apply so
- 00:47:08somehow if you use this as a numerical
- 00:47:09method you're you're in between you know
- 00:47:13statistical mechanics and and the true
- 00:47:16Dynamics somehow approach that's at
- 00:47:18least how I think of it and um and once
- 00:47:21you you have these things sorry let me
- 00:47:24just check the time so once you have
- 00:47:27these things you you can play a game the
- 00:47:29game is very fun you take whatever you
- 00:47:32want on the fluid side and you try to
- 00:47:34look at it on the Matrix side okay and
- 00:47:38then you get this dictionary and you can
- 00:47:39go the other way around you can say Okay
- 00:47:41Le theory is a very rich mathematical
- 00:47:44Theory maybe it has some tools that I
- 00:47:46can transfer back to the fluids so this
- 00:47:49is the game that uh I've been playing
- 00:47:52for several years together with milu
- 00:47:55Vivani who did his about this and uh one
- 00:47:59of the
- 00:48:00key results that Milo had in his thesis
- 00:48:03was that he in addition to using
- 00:48:06this uh this spatial discretization on
- 00:48:09the sphere he was able to find also a
- 00:48:12way to discretize this equation in time
- 00:48:15so that you preserve all the leoson
- 00:48:17structure Which is far from
- 00:48:19non-trivial so so so that was a very so
- 00:48:21we now have everything we need to
- 00:48:23preserve all the structure in the
- 00:48:25equations in on the computer except for
- 00:48:28round of Errors we still have round of
- 00:48:31Errors so you play this game you have
- 00:48:34verticity which corresponds to a matrix
- 00:48:36you have the cmir functions which
- 00:48:38corresponds to the integral corresponds
- 00:48:40to taking the trace so you have trace of
- 00:48:42of you know Matrix functions uh and then
- 00:48:45you have hamiltonian which just looks
- 00:48:47like this the values of the Omega this
- 00:48:50is a key point in quantum mechanics
- 00:48:53right the values of your function
- 00:48:55corresponds to the igen values of
- 00:48:56operator or I times the I values if it's
- 00:48:59a skew if it's a skew Herm missan
- 00:49:02Matrix uh and you we have this kind of
- 00:49:05interesting interpretation that the
- 00:49:07level sets of our proticity somehow
- 00:49:10corresponds to the igen vectors of the
- 00:49:13function okay so so you see it's natural
- 00:49:16to each smooth function you associate a
- 00:49:19level set level sets and values on that
- 00:49:22level sets corresponding to the value of
- 00:49:23the function in the same sense on The
- 00:49:25Matrix you have I
- 00:49:27values and to each igen value you
- 00:49:29associate one or in the generic case
- 00:49:31maybe just one igen
- 00:49:34vector okay so the we also get a lot of
- 00:49:38results from quantization Theory because
- 00:49:40this is a big field of mathematical
- 00:49:42physics so in particular we know that
- 00:49:45and you can even prove convergence here
- 00:49:47when n goes to Infinity the L Infinity
- 00:49:50Norm corresponds to the spectral norm
- 00:49:53and for example the L2 Norm corresponds
- 00:49:56to The Matrix forus Norm things like
- 00:49:59that uh here is something that mil and I
- 00:50:01was working with if you take like
- 00:50:03averages along the level set of the
- 00:50:06stream function so you take your
- 00:50:07verticity and then you take averages
- 00:50:09along the level sets of your stream
- 00:50:12function I mean you just think about
- 00:50:15that in the smooth setting it's kind of
- 00:50:18complicated but that's something that
- 00:50:20you want to do normally because it has
- 00:50:22to do with some smoothing and you know
- 00:50:24conver anyway so so on The Matrix side
- 00:50:27this is a very natural thing to do
- 00:50:29because you just project onto the
- 00:50:31stabilizer of your stream Matrix okay so
- 00:50:35yeah so now I I told you kind of what I
- 00:50:38why I think these two de Oiler equations
- 00:50:41are so beautiful I hope that I have one
- 00:50:43or two minutes more I will just show you
- 00:50:45some simulations as well uh for for
- 00:50:48these
- 00:50:49things and I mean so once Milo had
- 00:50:52developed this integrator we I mean we
- 00:50:54thought okay this is a nice publication
- 00:50:56in a good numerical Journal uh but we
- 00:50:59want more because we want to see what
- 00:51:01actually happens in the Dynamics so we
- 00:51:03just say okay let's start we do it on
- 00:51:05the sphere because that's what we did
- 00:51:06and let's start with some random
- 00:51:08randomly chosen but very smooth
- 00:51:10verticity field and run it through this
- 00:51:13numerical integrator that preserves all
- 00:51:14the structure and see what happens so we
- 00:51:16did this for for for many cases and and
- 00:51:20this is a typical thing that happens so
- 00:51:22you see we actually see
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