2012-02-14

I was inspired by a talk by Clayton Shonkwiler in the UGA topology seminar, on integral definitions of Milnor's triple linking number. What I have been thinking about is much simpler, just about the ordinary (double) linking number. There is an integral definition of this linking number (Gauss's integral) which is explained as the degree of the following map from $S^1 \times S^1 \to S^2$:

Given a $2$-component link $L$, realized by two disjoint embeddings $\phi_1, \phi_2 : S^1 \to \mathbb{R}^3$, we map $(\theta_1, \theta_2) \in S^1 \times S^1$ to $\phi_2(\theta_2) - \phi_1(\theta_1) / \| \phi_2(\theta_2) - \phi_1(\theta_1) \|$. Call this map $\Phi_L : T^2 \to S^2$. The degree of $\Phi_L$ is the only invariant needed to determine the homotopy class of $\Phi_L$. The linking number is a complete invariant of two-component links up to link homotopy (link homotopy means the individual components can cross themselves, but distinct components should remain distinct). I believe that, using some other easier definition of the linking number, there exists an easy direct proof of this fact that linking number determines link homotopy type.

So I believe that the logical conclusion of the above facts is that, for any $\Phi : T^2 \to S^2$, $\Phi$ is homotopic to $\Phi_L$ for some $L$ and, for any homotopy $\Phi_t$ from $\Phi_0 = \Phi_{L_0}$ to $\Phi_1 = \Phi_{L_1}$, there is a link homotopy $L_t$ such that the homotopy $\Phi_t$ is homotopic to $\Phi_{L_t}$. This is what I want to see directly and that is what I have been thinking about a bit.

The point is that an arbitrary $\Phi : T^2 \to S^2$ is not of the form $\Phi_L$ for a link $L$. The question is how to recover a candidate $L$ given $\Phi$.

If I can understand this then maybe I can understand the triple linking situation nicely and geometrically.

 

2012-02-01

Here is a fact: There is a measure of complexity of orientable surfaces, called genus, such that, if a surface $\Sigma$ if sufficiently complex (genus greater than $1$), then $\pi_1(\mathop{Diff}_0(\Sigma))=0$, where $\mathop{Diff}_0$ is the identity component of the self-diffeomorphism group. Is there any such measure of complexity in higher dimensions? Do "sufficiently complex" $3$-manifolds have $\pi_1(\mathop{Diff}_0) = 0$?

The contex for this question is the problem of recovering a smooth $n$-manifold from combinatorial data associated to a Morse $2$-function (generic smooth map to a $2$-manifold). If $\pi_1(\mathop{Diff}_0(F)) \neq 0$ for some regular fiber $F$, then in some sense we have no hope of writing down something combinatorial in the base that will determine the total space, because we can always remove a neighborhood $B^2 \times F$ of $F$ and glue it back in using a nontrivial loop of self-diffeomorphisms of $F$.

This issue in turn arose from (1) a paper Rob Kirby and I are writing and (2) discussions with Bruce Bartlett about his work with Chris Douglas, Chris Schommer-Pries and Jamie Vicary on the $1$-$2$-$3$ cobordism $2$-category. In the latter case, they understand this category by thinking about Morse $2$-functions on $3$-dimensional cobordisms between $2$-dimensional cobordisms; anyway, the regular fibers are disjoint unions of circles, and $\pi_1(\mathop{Diff}_0(S^1)) = \mathbb{Z}$, so the problem arises. But it seems it can be kept track of using knowledge about Dehn twists and the fact that the mapping class group of a surface is generated by Dehn twists.

Here is another question arising from my discussions with Bruce Bartlett: Is there a simple Morse/Cerf theory proof that the mapping class group of a surface is generated by Dehn twists (forget relations or finite presentations)? I would allow as input the facts that the mapping class group of a disk is trivial, that of a cylinder is generated by the Dehn twist about its core circle, and that of a pair of pants in which we allow the two cuffs to switch places is generated by Dehn twists and braid generators (half Dehn twists). My idea is then you pick your favorite Morse function $f$ on your surface and first argue (using the input facts above) that $f$-level-preserving automorphisms of the surface are generated by Dehn twists. Then you consider an arbitrary automorphism $\phi$ of the surface and consider a generic homotopy from $f$ to $f \circ \phi$. Then the decomposition of this homotopy into elementary moves (critical value crossings and births and deaths) should somehow fill in the rest of the picture.

 

Things to do with 120 dodecahedra

2011-12-06

Well it has been more than a year since I posted to this blog, which makes it not much of a blog. But I have big plans to get back to it, and to start the ball rolling: ...

I gave a math club talk a few weeks ago about the 120-cell, a 4-dimensional polytope with 120 dodecahedral facets. Here is the video taken by Eddie Beck of the UGA math club. Enjoy:  

Trivial homotopies between Morse functions

2010-12-01

This entry relates to a paper Katrin Wehreim, Chris Woodward and I are writing, and is also relevant to my forthcoming paper with Rob Kirby. I want to prove the following statement, which one would naturally assume is true but which is actually subtle, so I'm going to be very pedantic in the proof:

Theorem If $g_t \co X \to [0,1]$ is a $1$-parameter family of Morse functions on a cobordism $X$, with $g_t$ honestly Morse for all $t \in [0,1]$, with all critical values distinct, then there exist ambient isotopies $\phi_t \co I \to I$ and $\psi_t \co X \to X$ (fixed on boundaries and equal to the identity when $t=0$) such that $g_t = \phi_t \circ f_0 \circ \psi_t$.

Basically, the idea is that if you have a homotopy between Morse functions which "doesn't do anything", in the sense that there are no births or deaths of cancelling pairs of critical points and no crossings of critical values, then it really doesn't do anything in the sense that it can be realized by pre- and post-composing with ambient isotopies.

Proof First, because the critical values never cross and are all distinct, we can post-compose with an ambient isotopy $\alpha_t \co [0,1] \to [0,1]$ to arrange that the critical values are constant (independent of $t$). In other words, we replace $g_t$ with $f_t = \alpha_t \circ g_t$ so that, for each $t$, the critical values of $g_t$ are constants $c_1, \ldots, c_k$, independent of $t$. Now consider the function $F \co [0,1] \times X \to [0,1] \times [0,1]$ defined by $F(t,p) = (t,f_t(p))$. Note that the critical points of $F$ are pairs $(t,p)$ where $p$ is critical for $f_t$, that the set of critical points of $F$ is a collection of arcs in $[0,1] \times X$, and that along these arcs $DF$ has rank $1$. Furthermore, the image of each of these arcs is a horizontal line $[0,1] \times \{c_i\} \subset [0,1] \times [0,1]$, because the critical values of $f_t$ are independent of $t$. Thus the image of $DF$ at each critical point $(t,p)$ is spanned by $\partial_t \in T_{(t,f_t(p))} [0,1] \times [0,1]$.

I like to use coordinates $(t,z)$ on $[0,1] \times [0,1]$, since $t$ is "time" and $z$ is "height". This is a bit sloppy because I will also use the variable $t$ in the domain $[0,1] \times X$.

Now I claim that there exists a vector field $V$ on $[0,1] \times X$ such that $DF(V) = \partial_t$. To see this, we only need to argue that, around every point $(t_0,p_0) \in [0,1] \times X$, there is a ball $B$ in which such a vector field exists. After showing that such a vector field exists in each such ball, we can patch such vector fields together using a partition of unity, since, if $DF(V_1) = \ldots = DF(V_n) = \partial_t$ and $a_1 + \ldots + a_n =1$ then $DF(a_1 V_1 + \ldots + a_n V_n) = \partial_t$. When $(t_0,p_0)$ is a regular point for $F$, such a ball with such a vector field clearly exists since $DF$ is surjective. When $(t_0,p_0)$ is a critical point, with critical value $(t_0,c_i=f_{t_0}(p_0))$, note that we can find coordinates $(x_1, \ldots, x_n)$ in a neighborhood of $p_0 \in X$, depending smoothly on $t$, with respect to which $f_t(x_1, \ldots, x_n) = c_i + \sum \pm x_j^2$ (Here we are using the fact that the critical values of $f_t$ are independent of $t$). This translates into coordinates $(t',x_1,\ldots,x_n)$ on a neighborhood of $(t_0,p_0) \in [0,1] \times X$ with respect to which $F(t',x_1,\ldots,x_n) = (t',c_i+\sum \pm x_j^2)$, and thus we can take $V = \partial_{t'}$ in this coordinate system.

(Note: I am appealing to a parametrized version of the Morse lemma, that nondenerate critical points are standard. Perhaps this should be written down also, to be very precise, but since the Morse lemma boils down to Taylor's theorem and Gram-Schmidt orthonormalization, both of which behave smoothly with respect to a parameter, this should be obvious, right?)

At this point the reader can probably see the end of the proof, but just to be totally pedantic, here it is (the trick to actually writing it down is getting the isotopies going in the right directions):

Now that we have this vector field $V$, note that $DF(V) = \partial_t$ means that flow along $V$ in $[0,1] \times X$ preserves the height function $z \circ F$, where $z \circ F(t,p) = f_t(p)$. We also know that $V = \partial_t + V_X$, where $V_X$ is tangent to $\{t\} \times X$. Thus $V_X$ is actually a time-dependent vector field $W(t)$ on $X$, and thus flow along $V$ turns into flow along $W(t)$ which gives an isotopy $\beta_t \co X \to X$. The fact that flow along $V$ preserves $z \circ F(t,p) = f_t(p)$ means that when we pull $f_t$ back via the flow $\beta_t$ along $W(t)$ we get $f_0$. I.e. $f_0 = f_t \circ \beta_t$.

Now recall that $f_t = \alpha_t \circ g_t$, and $f_0 = g_0$ because all our isotopies start with the identity. We want $g_t = \phi_t \circ g_0 \circ \psi_t$. Well, $g_t = \alpha_t^{-1} \circ f_t = \alpha_t^{-1} \circ f_0 \circ \beta_t^{-1} = \alpha_t^{-1} \circ g_0 \circ \beta_t^{-1}$, so we let $\phi_t = \alpha_t^{-1}$ and $\psi_t = \beta_t^{-1}$.

QED (I don't know an html symbol for a little square.)