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authorJaron Kent-Dobias <jaron@kent-dobias.com>2022-02-02 21:21:41 +0100
committerJaron Kent-Dobias <jaron@kent-dobias.com>2022-02-02 21:21:41 +0100
commite95106056fe738564a4e57fcdfad81e4799e47de (patch)
tree93c60493d9429afa80729b00cdbef50dea1cebbe
parentba657f5720db080f1120e93cdf20098c844ccbe6 (diff)
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Some writing and editing.
-rw-r--r--stokes.tex23
1 files changed, 10 insertions, 13 deletions
diff --git a/stokes.tex b/stokes.tex
index 2edf7cc..230ed01 100644
--- a/stokes.tex
+++ b/stokes.tex
@@ -288,10 +288,8 @@ holomorphic property of $\mathcal S$:
\|\partial\mathcal S\|^2-(\|\partial\mathcal S\|^*)^2
\right)=0.
\end{eqnarray}
-As a result of this conservation law, surfaces of constant imaginary action
-will be important when evaluting the possible endpoints of trajectories. A
-consequence of this conservation is that the flow in the action takes a simple
-form:
+A consequence of this conservation is that the flow in the action takes a
+simple form:
\begin{equation}
\dot{\mathcal S}
=\dot z\partial\mathcal S
@@ -301,22 +299,21 @@ form:
In the complex-$\mathcal S$ plane, dynamics is occurs along straight lines in
a direction set by the argument of $\beta$.
-Let us consider the generic case, where the critical points of $\mathcal S$ have
-distinct energies. What is the topology of the $C=\operatorname{Im}\mathcal S$ level
-set? We shall argue its form by construction. Consider initially the situation
-in the absence of any critical point. In this case the level set consists of a
-single simply connected surface, locally diffeomorphic to $\mathbb R^{2D-1}$. Now, `place' a generic
-(nondegenerate) critical point in the function at $z_0$. In the vicinity of the critical
-point, the flow is locally
+What does the topology of the space of thimbles look like? Let us consider the
+generic case, where the critical points of $\beta\mathcal S$ have distinct
+energies. Consider initially the situation in the absence of any critical
+point, e.g., as for a constant or linear function. Now, `place' a generic
+(nondegenerate) critical point in the function at $z_0$. In the vicinity of the
+critical point, the flow is locally
\begin{equation}
\dot z
- \simeq-\frac12(\partial\partial\mathcal S|_{z=z_0})^\dagger P(z-z_0)^*
+ \simeq-\frac{\beta^*}2(\partial\partial\mathcal S|_{z=z_0})^\dagger P(z-z_0)^*
\end{equation}
The matrix $(\partial\partial\mathcal S)^\dagger P$ has a spectrum identical to that of
$(\partial\partial\mathcal S)^\dagger$ save marginal directions corresponding to the normals to
manifold. Assuming we are working in a diagonal basis, this becomes
\begin{equation}
- \dot z_i=-\frac12\lambda_i\Delta z_i^*+O(\Delta z^2,(\Delta z^*)^2)
+ \dot z_i=-\frac12(\beta\lambda_i)^*\Delta z_i^*+O(\Delta z^2,(\Delta z^*)^2)
\end{equation}
Breaking into real and imaginary parts gives
\begin{eqnarray}