Files
optimiz-rs/docs/source/theory/mathematical_foundations.md
T
ThotDjehuty b41618c627 docs(theory): enrich Section 4 optimal control with 4 worked examples
- Add HJB/PMP/HJBI comparison overview table
- Add Merton 1969 portfolio allocation example (log-utility, constant fraction)
- Add Almgren-Chriss inventory liquidation example (LQR + TWAP-like schedule)
- Add PMP costate derivation for Merton problem
- Add American option as viscosity example (variational inequality, smooth-pasting)
- Explain jump integral term intuition in HJBI
- Add shooting method pseudocode for PMP
- Mirror all enrichments in LaTeX .tex source
- Regenerate PDF (13 pages, cross-refs resolved)
2026-03-06 20:22:35 +01:00

30 KiB
Raw Blame History

Mathematical Foundations

This page develops the core mathematics underlying Optimiz-rs's Rust kernels — from first principles through advanced theory. Each section opens with a definition block, builds intuition through examples, and closes with a notebook micro-check. For complete walkthroughs see examples/notebooks/.


1 · Differential Evolution (DE)

Background

DE is a gradient-free population-based optimizer for f: \mathbb{R}^d \to \mathbb{R}, not required to be smooth or convex. At generation g we maintain N candidate solutions \{\mathbf{x}_{i,g}\} \subset \mathbb{R}^d.

Key insight: The difference vector \mathbf{x}_{r_2}-\mathbf{x}_{r_3} is an unbiased directional finite-difference of f, so DE implicitly estimates curvature without Jacobians.

Operators

Step Formula Role
Mutation (rand/1) \mathbf{v}_{i,g} = \mathbf{x}_{r_1} + F(\mathbf{x}_{r_2}-\mathbf{x}_{r_3}) explore
Binomial crossover u_{i,j} = v_{i,j} if U(0,1)<CR or j=j_\text{rand} mix dimensions
Greedy selection \mathbf{x}_{i,g+1} = \mathbf{u}_{i,g} iff f(\mathbf{u})\le f(\mathbf{x}) exploit

Convergence (informal): Under bounded population diversity and Lipschitz f, the best-so-far value converges a.s. to a stationary point as N,g\to\infty (Price et al. 2005).

Self-Adaptive jDE (Optimiz-rs default)

Parameters F,CR are per-individual and reset stochastically each generation:


F_i^{g+1} = \begin{cases} F_{\min} + r_1 F_{\max} & r_2 < \tau_1,\\ F_i^g & \text{otherwise,}\end{cases}
\qquad
CR_i^{g+1} = \begin{cases} U(0,1) & r_3 < \tau_2,\\ CR_i^g & \text{otherwise.}\end{cases}

\tau_1=\tau_2=0.1 by default. On rugged landscapes this produces bimodal F histograms concentrated near 0.8 — a sign the landscape is highly multimodal.

Notebook check (05_performance_benchmarks.ipynb): Plot F_i, CR_i histograms every 50 generations; expect values clustering in [0.5,0.9] on hard problems.


2 · Stochastic Processes

These form the probabilistic backbone of all continuous-time models in Optimiz-rs.

2.1 Brownian Motion

::::{admonition} Definition — Wiener Process :class: definition

A stochastic process W = (W_t)_{t\ge 0} on (\Omega,\mathcal{F},\mathbb{P}) is a standard Brownian motion if:

  1. W_0 = 0 a.s.
  2. Increments are independent: W_t - W_s \perp \mathcal{F}_s for t>s.
  3. W_t - W_s \sim \mathcal{N}(0, t-s) for all 0\le s<t.
  4. Paths t\mapsto W_t(\omega) are continuous a.s. ::::

Key properties:

  • \mathbb{E}[W_t] = 0, \operatorname{Var}(W_t) = t, \operatorname{Cov}(W_s,W_t) = \min(s,t).
  • Quadratic variation: [W]_T = T (paths are non-differentiable but have finite $p$-variation for p>2).
  • Self-similarity: c^{-1/2}W_{ct} \overset{d}{=} W_t (Hurst exponent H=\tfrac12).

Example — Geometric BM: S_t = S_0 \exp\!\bigl((\mu-\tfrac12\sigma^2)t + \sigma W_t\bigr) is the BlackScholes price model. Sample path sketch:

S_t
|       .---.
|  .--./     \----.
| /                \---------.
|/
+-------------------------------> t
  0             T
(log-normal marginals; continuous, nowhere-differentiable paths)

2.2 Itô Calculus

::::{admonition} Definition — Itô Integral :class: definition

For adapted f \in \mathcal{L}^2 (i.e. \mathbb{E}\!\int_0^T f_t^2\,dt < \infty):

\int_0^T f_t\,dW_t \;=\; L^2\text{-}\lim_{|\pi|\to 0} \sum_{k} f_{t_k}(W_{t_{k+1}}-W_{t_k}).

The Itô integral is a martingale with zero mean and Itô isometry \mathbb{E}\bigl[(\int_0^T f_t\,dW_t)^2\bigr] = \mathbb{E}\int_0^T f_t^2\,dt. ::::

::::{admonition} Theorem — Itô's Lemma :class: tip

For dX_t = \mu_t\,dt + \sigma_t\,dW_t and F \in C^{1,2}([0,T]\times\mathbb{R}):

dF(t,X_t) = \partial_t F\,dt + \partial_x F\,dX_t + \tfrac{1}{2}\partial_{xx}F\,\sigma_t^2\,dt.

The correction term \tfrac12\sigma^2\partial_{xx}F (absent in ordinary calculus) arises from the non-zero quadratic variation d[W]_t = dt. ::::

Example: Let X_t = \log S_t with dS_t = \mu S_t\,dt + \sigma S_t\,dW_t. Itô's Lemma gives dX_t = (\mu - \tfrac12\sigma^2)\,dt + \sigma\,dW_t. ✔

2.3 General Itô SDEs

dX_t = b(t, X_t)\,dt + \boldsymbol{\sigma}(t, X_t)\,dW_t,\quad X_0 = x_0.

Existence & uniqueness (PicardLindelöf for SDEs): If b, \boldsymbol{\sigma} are globally Lipschitz with linear growth, there exists a unique strong solution with \mathbb{E}[\sup_{t\le T}\|X_t\|^2]<\infty.

Common SDE Models

Process SDE Stationary distribution
Brownian motion dX = \sigma\,dW
Geometric BM dX = \mu X\,dt + \sigma X\,dW log-normal
OrnsteinUhlenbeck dX = \kappa(\theta-X)\,dt + \sigma\,dW \mathcal{N}(\theta, \sigma^2/2\kappa)
CIR dX = \kappa(\theta-X)\,dt + \sigma\sqrt{X}\,dW Gamma$(2\kappa\theta/\sigma^2, \sigma^2/2\kappa)$

2.4 Ornstein-Uhlenbeck (Mean-Reversion)

Used in Optimiz-rs's sparse_mean_reversion and ou_estimator modules:

dX_t = \kappa(\theta - X_t)\,dt + \sigma\,dW_t.

Closed-form solution:

X_t = \theta + (X_0 - \theta)e^{-\kappa t} + \sigma\int_0^t e^{-\kappa(t-s)}\,dW_s.

Half-life: \tau_{1/2} = \ln 2/\kappa. With $\kappa=0.2$/day, half-life ≈ 3.5 days — typical for equity-pair spreads.

MLE log-likelihood (discrete observations at spacing \Delta t):

$$\ell(\kappa,\theta,\sigma) = -\frac{1}{2}\sum_{i=1}^{n}\left[\log(2\pi\hat\sigma_i^2)

  • \frac{(X_{t_i} - \hat\mu_i)^2}{\hat\sigma_i^2}\right],$$

where \hat\mu_i = \theta + (X_{t_{i-1}}-\theta)e^{-\kappa\Delta t} and \hat\sigma_i^2 = \frac{\sigma^2}{2\kappa}(1-e^{-2\kappa\Delta t}).


3 · Jump Processes

Many financial time series exhibit sudden large moves that Brownian motion cannot capture.

3.1 Poisson Process

::::{admonition} Definition — Poisson Process :class: definition

A counting process N = (N_t)_{t\ge 0} is a Poisson process with intensity \lambda > 0 if:

  1. N_0 = 0.
  2. Independent, stationary increments.
  3. \mathbb{P}(N_{t+h}-N_t=1) = \lambda h + o(h) and \mathbb{P}(\Delta N > 1) = o(h). ::::

Equivalently, N_t \sim \text{Poisson}(\lambda t) and inter-arrival times are \text{Exp}(\lambda). The compensated process \tilde N_t = N_t - \lambda t is a martingale.

3.2 Compound Poisson Jump-Diffusion (Merton 1976)

\frac{dS_t}{S_{t^-}} = \mu\,dt + \sigma\,dW_t + d\Bigl(\sum_{k=1}^{N_t}(e^{J_k}-1)\Bigr),

with N_t Poisson(\lambda) and J_k \sim \mathcal{N}(\mu_J, \sigma_J^2).

Merton option price — a Poisson mixture of BlackScholes prices:

$$C_{\text{Merton}} = \sum_{n=0}^\infty \frac{e^{-\lambda' T}(\lambda' T)^n}{n!} \cdot C_{\text{BS}}!\left(S_0, K, T, r_n, \sigma_n^2\right),$$

where \lambda' = \lambda e^{\mu_J+\frac12\sigma_J^2}, r_n = r - \lambda(e^{\mu_J+\frac12\sigma_J^2}-1) + n(\mu_J+\tfrac12\sigma_J^2)/T, and \sigma_n^2 = \sigma^2 + n\sigma_J^2/T.

3.3 Lévy Processes and the LévyKhintchine Representation

::::{admonition} Theorem — LévyKhintchine :class: tip

Every Lévy process (independent stationary increments) has characteristic function

$$\mathbb{E}[e^{i\xi X_t}] = \exp!\Bigl(t\Bigl[i b\xi - \tfrac{1}{2}\sigma^2\xi^2

  • \int_{\mathbb{R}\setminus{0}} \bigl(e^{i\xi z}-1-i\xi z\mathbf{1}_{|z|\le1}\bigr)\nu(dz)\Bigr]\Bigr)$$

where (b, \sigma^2, \nu) is the Lévy triplet and \nu the Lévy measure, satisfying \int(1\wedge z^2)\nu(dz)<\infty. ::::

Lévy Process Zoo

Process Lévy measure \nu Use case
Brownian motion \nu=0 continuous diffusion
Compound Poisson finite measure rare large jumps
Variance Gamma \nu(dz)\propto e^{-c\|z\|}/\|z\| equity returns
CGMY e^{-G\|z\|}/\|z\|^{1+Y} (neg), e^{-Mx}/x^{1+Y} (pos) heavy tails, Y\in(0,2)
$\alpha$-stable c\|z\|^{-1-\alpha} infinite-variance regimes

3.4 SDEs with Jumps — Generator and Itô Formula

$$dX_t = b(X_{t^-}),dt + \sigma(X_{t^-}),dW_t

  • \int_{\mathbb{R}} c(X_{t^-}, z),\tilde N(dt, dz),$$

where \tilde N(dt,dz) = N(dt,dz) - \nu(dz)\,dt is the compensated jump measure.

Itô formula for jump-diffusions:

$$dF(X_t) = \mathcal{L}F,dt + \partial_x F,\sigma,dW_t

  • \int\bigl[F(X_{t^-}+c)-F(X_{t^-})\bigr]\tilde N(dt,dz),$$

where the generator is

$$\mathcal{L}F = b,\partial_x F + \tfrac12\sigma^2\partial_{xx}F

  • \int\bigl[F(x+c)-F(x)-c,\partial_x F\bigr]\nu(dz).$$

4 · Optimal Control (HJB, PMP, Jumps)

Big picture. Optimal control asks: given a stochastic system we can steer with a control u_t, what policy minimises expected cost? Three complementary tools answer this:

Tool Solves Scales to Intuition
HJB PDE Value function V(t,x) Low dim (PDE grid) Dynamic programming
PMP Optimal paths (X_t,p_t) High dim (ODE) Adjoint sensitivity
HJBI Same as HJB + jumps Low dim Non-local integral term

4.1 Stochastic HJB

Setup. The state X_t \in \mathbb{R}^d evolves as

dX_t = b(X_t,u_t)\,dt + \sigma(X_t,u_t)\,dW_t,

and we minimise the total expected cost

J(t,x;u) = \mathbb{E}\!\left[\int_t^T \ell(X_s,u_s)\,ds + g(X_T)\,\Big|\,X_t=x\right].

The value function V(t,x) = \inf_u J(t,x;u) satisfies:

$$-\partial_t V = \inf_{u\in\mathcal{U}}\Bigl[\ell(x,u) + \nabla_x V^{!\top} b(x,u)

  • \tfrac12\operatorname{Tr}\bigl(\sigma\sigma^{!\top}(x,u),\nabla_x^2 V\bigr)\Bigr], \quad V(T,\cdot)=g.$$

Intuition. The three terms inside the infimum are:

  • \ell(x,u) — instantaneous running cost (pay now),
  • \nabla_x V^\top b — drift of the value (first-order)
  • \tfrac12\operatorname{Tr}(\sigma\sigma^\top\nabla^2 V) — curvature correction due to noise (the stochastic analogue of a second-order Taylor term).

Under smooth V, the feedback law is u^\star(t,x) = \arg\min_u[\ell(x,u)+\nabla_x V^\top b(x,u)].


::::{admonition} Example — Optimal Portfolio Allocation :class: note

Investor wealth X_t follows dX_t = (r + u_t(\mu-r))X_t\,dt + u_t\sigma X_t\,dW_t, where u_t\in\mathbb{R} is the fraction invested in the risky asset.

Minimise -\mathbb{E}[\log X_T] (maximise expected log-utility).

Ansatz: V(t,x) = \ln x + f(t). Substituting into HJB:

f'(t) = -r - \frac{(\mu-r)^2}{2\sigma^2},\qquad f(T)=0.

The optimal Merton rule is constant:

u^\star = \frac{\mu-r}{\sigma^2} \quad (\text{fraction in risky asset}).

This is the classic Merton (1969) result: invest a fixed fraction proportional to the Sharpe ratio and inversely to variance — independent of wealth and time. ::::


LQR special case (\ell = x^\top Q x + u^\top R u, b=Ax+Bu, \sigma constant): V(t,x)=x^\top P(t)x + v(t) with P solving the matrix Riccati ODE:

-\dot P = A^\top P + PA - PBR^{-1}B^\top P + Q,\quad P(T)=Q_T.

The optimal control is linear feedback: u^\star_t = -R^{-1}B^\top P(t)X_t.


::::{admonition} Example — Optimal Inventory (AlmgrenChriss liquidation) :class: note

A trader must liquidate X_0 shares by time T. Inventory X_t, trading rate u_t<0:

$$dX_t = u_t,dt, \quad \ell(x,u) = \underbrace{\alpha x^2}{\text{risk}} + \underbrace{\beta u^2}{\text{impact}}.$$

This is a deterministic LQR (\sigma=0) with A=0, B=1, Q=\alpha, R=\beta. The Riccati solution gives the TWAP-like schedule

$$u^\star(t,x) = -\frac{\alpha}{\beta}\cdot\frac{\sinh(\kappa(T-t))}{\sinh(\kappa T)}\cdot X_0, \quad \kappa=\sqrt{\alpha/\beta}.$$

Large \kappa (high risk aversion or low impact cost) → aggressive front-loaded selling. ::::


4.2 Pontryagin Maximum Principle

The PMP avoids the curse of dimensionality — it converts the HJB PDE into a two-point boundary-value ODE in (X_t, p_t), making it feasible in high dimensions where a PDE grid is intractable.

::::{admonition} Theorem (PMP) :class: tip

Define the Hamiltonian \mathcal{H}(x,u,p) = \ell(x,u)+p^\top b(x,u). If (X^\star, u^\star) is optimal, there exists a costate (adjoint) process p_t with:

\dot p_t = -\nabla_x \mathcal{H}(X_t^\star, u_t^\star, p_t),\quad p_T = \nabla_x g(X_T^\star),

and the optimality condition u_t^\star = \arg\min_u \mathcal{H}(X_t^\star, u, p_t) holds a.e. ::::

Costate intuition. p_t is the shadow price of state X_t:

p_t = \nabla_x V(t, X_t^\star) = \frac{\partial (\text{optimal cost-to-go})}{\partial x}.

Increasing the current state by dx changes future cost by p_t^\top dx. This is exactly the adjoint/backpropagation equation of deep learning — PMP is the continuous-time version of gradient backpropagation through a dynamical system.

Algorithm (shooting method):

1. Guess costate p_0
2. Integrate forward:  dX = b(X, u*(X,p)) dt           (state ODE)
3. Integrate backward: dp = -∇_x H(X, u*, p) dt        (costate ODE)
4. Check boundary condition:  p_T = ∇g(X_T)
5. If not satisfied -> update p_0 (Newton / gradient) -> go to 2

::::{admonition} Example — PMP for the Merton Problem :class: note

With \ell = 0, g(x) = -\ln x, b = (r+u(\mu-r))x, \sigma^\top\sigma = u^2\sigma^2 x^2, the Hamiltonian is \mathcal{H}(x,u,p) = p(r+u(\mu-r))x.

Costate ODE: \dot p_t = -\partial_x \mathcal{H} = -p_t(r+u^\star(\mu-r)), with terminal p_T = -1/X_T^\star.

Optimality condition \partial_u\mathcal{H}=0 gives p_t(\mu-r)x + \partial_u(\tfrac12\sigma^2 u^2 x^2 \partial_{xx}V)=0, recovering u^\star = (\mu-r)/\sigma^2 as before.

The costate path p_t = -e^{-(T-t)(r+(\mu-r)u^\star)}/X_t^\star confirms that the shadow price scales inversely with wealth. ::::


The costate pair (X_t^\star, p_t) moves along Hamiltonian geodesics on T^\star\mathbb{R}^d — a direct link to symplectic geometry (§10.4).


4.3 HJB with Jumps (HJBI)

When the state can jump (§3.4), the HJB equation gains a non-local integral operator:

$$-\partial_t V = \inf_{u}\Bigl[\ell + \nabla V^\top b + \tfrac12\operatorname{Tr}(\sigma\sigma^\top\nabla^2 V)

  • \underbrace{\int\bigl[V(x+c(x,u,z))-V(x)-\nabla V^\top c(x,u,z)\bigr]\nu(dz)}_{\text{expected value change from jumps}}\Bigr].$$

Intuition for the integral term. A jump of size c moves the state from x to x+c, changing the value function by V(x+c)-V(x). The compensator \nabla V^\top c subtracts the linear part already counted in the drift, following Itô's formula for jump processes (§3.4).

The optimal_control module discretises the integral on a truncated support [-z_{\max}, z_{\max}] using Gaussian quadrature.


::::{admonition} Example — Optimal Execution with Jump Risk :class: note

Extend the inventory model with Poisson order-flow shocks:

dX_t = u_t\,dt + \Delta J_t,\quad \Delta J_t \sim \text{Compound Poisson}(\lambda, \mathcal{N}(0,\sigma_J^2)).

The HJBI becomes:

$$-\partial_t V = \inf_u\Bigl[\alpha x^2 + \beta u^2 + \partial_x V,u

  • \lambda,\mathbb{E}_z[V(x+z)-V(x)-z,\partial_x V]\Bigr].$$

With Gaussian jumps, the expectation computes as \lambda(\tfrac12\sigma_J^2\,\partial_{xx}V), so the HJBI reduces to the same LQR Riccati ODE but with effective diffusion \sigma_{\text{eff}}^2 = \lambda\sigma_J^2.

Key insight: order-flow risk acts like additional Brownian volatility, accelerating the optimal sell schedule. ::::


4.4 Viscosity Solutions

When V fails to be C^{1,2} — which happens with degenerate diffusion (\sigma \approx 0), state/control constraints, or non-smooth terminal conditions — classical solutions may not exist. Viscosity solutions (CrandallLions 1983) provide a rigorous weak notion that restores existence and uniqueness.

Why they matter: In practice, HJB is solved on a grid and V is only piecewise smooth. Viscosity theory guarantees the numerical scheme converges to the true solution.

::::{admonition} Definition — Viscosity Subsolution :class: definition

A continuous V is a viscosity subsolution if for every smooth \phi touching V from above at (t_0,x_0) (i.e., V - \phi has a local maximum there):

-\partial_t\phi(t_0,x_0) \le \inf_u\Bigl[\ell(x_0,u) + \nabla_x\phi^\top b + \tfrac12\operatorname{Tr}(\sigma\sigma^\top\nabla^2\phi)\Bigr].

A supersolution reverses the inequality with a smooth test touching from below. The unique viscosity solution is simultaneously both. ::::

Practical interpretation. Classical calculus says "V satisfies the PDE pointwise." Viscosity theory says "V satisfies the PDE in an averaged sense via test functions — even at kinks." The condition prevents V from being arbitrarily steep or flat at non-smooth points.

Optimiz-rs's backward DP converges to the viscosity solution under the CFL condition \Delta t \le C\,(\Delta x)^2.


::::{admonition} Example — American Option as a Viscosity Problem :class: note

An American put has early-exercise payoff g(x) = (K-x)^+. The value function satisfies the variational inequality (a two-region HJB):

\min\Bigl(-\partial_t V - \mathcal{L}_{\text{BS}}V,\; V - (K-x)^+\Bigr) = 0,

where \mathcal{L}_{\text{BS}}V = rx\partial_x V + \tfrac12\sigma^2 x^2\partial_{xx}V - rV.

  • Continuation region (V > (K-x)^+): the BlackScholes PDE holds.
  • Exercise region (V = (K-x)^+): the option is exercised immediately.

At the free boundary the gradient \partial_x V is continuous (smooth-pasting) but \partial_{xx}V is not — so V is only C^1, not C^2. Viscosity theory handles this kink rigorously. ::::

Backward DP grid schema:

t=T    [ g(x_1)  g(x_2)  ...  g(x_n) ]   terminal condition
t=T-1  [ V^1     V^2     ...  V^n    ]   one backward step
 .
 .
t=0    [ V_0^1   V_0^2   ...  V_0^n  ]  -> optimal policy u*(x,0)

5 · Mean Field Games (1D Solver)

MFG couples a backward HJB (individual value) with a forward FokkerPlanck (population density):

$$\begin{aligned} \text{HJB (backward): } & -\partial_t u - \nu\partial_{xx}u + H(x,\partial_x u, m) = 0, & u(T,x)&=g(x),\ \text{FokkerPlanck (forward): } & \partial_t m - \nu\partial_{xx}m - \partial_x(m,\partial_p H) = 0, & m(0,x)&=m_0(x). \end{aligned}$$

Coupling: H depends on m (mean-field interaction), creating a fixed-point problem.

Fixed-point algorithm:

1. Initialise m^0 = m_0  (e.g. Gaussian)
2. Solve HJB backward  -> u^{k+1}
3. Extract optimal drift: alpha*(x,t) = -d_p H(x, d_x u^{k+1}, m^k)
4. Solve Fokker-Planck forward with alpha* -> m^{k+1}
5. Check ||m^{k+1} - m^k||_1 < eps; if not, k++ -> go to 2

Convergence: For monotone coupling (LasryLions 2007), the system has a unique solution and the fixed-point iteration contracts.

Practical tip: Monitor both \|m^{k+1}-m^k\|_1 and \|u^{k+1}-u^k\|_\infty; divergence of either signals non-monotone coupling or too large a time step.


6 · Kalman Filtering

6.1 Linear-Gaussian State Space

$$\mathbf{x}t = F\mathbf{x}{t-1} + \mathbf{w}_t,; \mathbf{w}_t\sim\mathcal{N}(0,Q); \qquad \mathbf{y}_t = H\mathbf{x}_t + \mathbf{v}_t,; \mathbf{v}_t\sim\mathcal{N}(0,R).$$

Predict:

\hat{\mathbf{x}}^-_t = F\hat{\mathbf{x}}_{t-1},\quad P^-_t = FP_{t-1}F^\top+Q.

Update:

$$K_t = P^-_t H^\top(HP^-_t H^\top + R)^{-1},\quad \hat{\mathbf{x}}_t = \hat{\mathbf{x}}^-_t + K_t(\mathbf{y}_t - H\hat{\mathbf{x}}^-_t),\quad P_t = (I-K_t H)P^-_t.$$

K_t is the Kalman gain — it interpolates between full prior trust (K\to0) and full observation trust (K\to H^{-1}).

6.2 Information-Theoretic View

The Kalman filter computes the exact conditional mean \hat{\mathbf{x}}_t = \mathbb{E}[\mathbf{x}_t \mid \mathbf{y}_{1:t}] in Gaussian models and minimises D_{\mathrm{KL}}(p(\mathbf{x}_t|\mathbf{y}_{1:t})\,\|\,\mathcal{N}(\hat{\mathbf{x}}_t, P_t)) over all Gaussian approximations.

6.3 Continuous-Time Limit (KalmanBucy)

For d\mathbf{X}_t = A\mathbf{X}_t\,dt + B\,d\mathbf{W}_t, d\mathbf{Y}_t = C\mathbf{X}_t\,dt + d\mathbf{V}_t, the error covariance satisfies the Riccati ODE:

\dot P = AP + PA^\top + BQB^\top - PC^\top R^{-1}CP,\qquad P(0)=P_0,

which converges to the algebraic Riccati solution at steady state.


7 · MCMC (MetropolisHastings and Langevin)

7.1 MetropolisHastings

For target \pi(x) \propto e^{-U(x)} and proposal q(x'\mid x):

\alpha(x\to x') = \min\!\Bigl(1, \frac{\pi(x')q(x\mid x')}{\pi(x)q(x'\mid x)}\Bigr).

Detailed balance \pi(x)\alpha(x\to x') = \pi(x')\alpha(x'\to x) ensures \pi is the unique stationary distribution.

Optimal scaling: With Gaussian proposal q(x'|x)=\mathcal{N}(x,h^2 I_d), step h^\star \approx 2.38/\sqrt{d} (RobertsGelmanGilks 1997) targets ~2345 % acceptance.

7.2 Langevin Dynamics (MALA)

Metropolis-Adjusted Langevin proposal:

x' = x - \tfrac{h^2}{2}\nabla U(x) + h\,\xi, \quad \xi\sim\mathcal{N}(0,I_d),

a discretisation of the overdamped Langevin SDE:

dX_t = -\nabla U(X_t)\,dt + \sqrt{2}\,dW_t,

whose stationary distribution is exactly \pi \propto e^{-U} (FokkerPlanck analysis).

MALA converges in O(d^{1/3}) steps vs O(d) for RW-MH — a key advantage for high-dimensional posteriors.

Heuristic: Tune proposal std so acceptance is ~2545 %; see examples/notebooks/02_mcmc.ipynb for trace plots.


8 · Hidden Markov Models (HMM)

8.1 Model

Latent Markov chain Z_t \in \{1,\ldots,K\} with transition matrix A_{ij}=\mathbb{P}(Z_t=j\mid Z_{t-1}=i) generates observations Y_t \mid Z_t=k \sim B_k(y).

8.2 BaumWelch (EM)

E-step (forwardbackward):

$$\alpha_t(k) = B_k(y_t)\sum_j \alpha_{t-1}(j)A_{jk}, \qquad \beta_t(k) = \sum_j A_{kj}B_j(y_{t+1})\beta_{t+1}(j).$$

$$\gamma_t(k) = \frac{\alpha_t(k)\beta_t(k)}{\sum_j \alpha_t(j)\beta_t(j)}, \qquad \xi_t(j,k) = \frac{\alpha_t(j)A_{jk}B_k(y_{t+1})\beta_{t+1}(k)}{\mathcal{L}}.$$

M-step:

$$\hat A_{jk} = \frac{\sum_t \xi_t(j,k)}{\sum_t\gamma_t(j)}, \qquad \hat\mu_k = \frac{\sum_t \gamma_t(k),y_t}{\sum_t \gamma_t(k)}.$$

Information-theoretic view: BaumWelch is EM on the complete-data log-likelihood; each iteration monotonically increases \mathcal{L}(\theta) by Jensen's inequality.

Viterbi (MAP path): Replace sum-product with max-product: \delta_t(k) = \max_j \delta_{t-1}(j)A_{jk} \cdot B_k(y_t), runs in O(TK^2).

Quality check: Log-likelihood per EM iteration must be non-decreasing; a confusion matrix of Viterbi labels vs. ground truth validates regime recovery.


9 · Information Theory

9.1 Entropy and KL Divergence

::::{admonition} Definition — KL Divergence :class: definition

For densities p, q:

D_{\mathrm{KL}}(p\,\|\,q) = \int p(x)\log\frac{p(x)}{q(x)}\,dx \;\ge\; 0,

with equality iff p=q a.e. (Gibbs' inequality). Non-symmetric. ::::

Connection to model selection: AIC = 2k - 2\ln\hat{\mathcal{L}} and BIC = k\ln n - 2\ln\hat{\mathcal{L}} bound D_{\mathrm{KL}}(p_{\text{true}}\,\|\,p_\theta).

9.2 Fisher Information

::::{admonition} Definition — Fisher Information Matrix :class: definition

For parametric model p(x;\theta):

$$\mathcal{I}(\theta){ij} = \mathbb{E}{x\sim p}!\left[\partial_{\theta_i}\log p;\partial_{\theta_j}\log p\right] = -\mathbb{E}!\left[\partial^2_{\theta_i\theta_j}\log p\right].$$ ::::

CramérRao bound: Any unbiased estimator \hat\theta satisfies \operatorname{Cov}(\hat\theta) \succeq \mathcal{I}(\theta)^{-1}. MLE achieves equality asymptotically.

Example — Gaussian HMM emission B_k = \mathcal{N}(\mu_k,\sigma_k^2): \mathcal{I}(\mu_k)=\sigma_k^{-2}, \mathcal{I}(\sigma_k^2)=(2\sigma_k^4)^{-1}.

9.3 Mutual Information and Feature Relevance

I(X;Y) = D_{\mathrm{KL}}\bigl(p(X,Y)\,\|\,p(X)p(Y)\bigr) = H(X) - H(X\mid Y) \ge 0.

mRMR criterion (minimum redundancy, maximum relevance) for the sparse module:

\max_{Y_i} \Bigl[I(Y_i;\text{target}) - \frac{1}{|S|}\sum_{Y_j\in S}I(Y_i;Y_j)\Bigr].

9.4 Natural Gradient (Preview)

Classical gradient descent ignores the geometry of parameter space. The natural gradient replaces \nabla_\theta\mathcal{L} with \mathcal{I}(\theta)^{-1}\nabla_\theta\mathcal{L}, giving a reparametrisation-invariant update — see §10.2 for the full geometric development.


10 · Differential Geometry

10.1 Riemannian Manifolds

::::{admonition} Definition — Riemannian Manifold :class: definition

A Riemannian manifold (M, g) is a smooth manifold M with a metric tensor g_p: a symmetric, positive-definite bilinear form on each tangent space T_p M. ::::

Geodesics (locally shortest paths) satisfy:

\ddot\gamma^k + \sum_{i,j}\Gamma^k_{ij}\,\dot\gamma^i\dot\gamma^j = 0,

where \Gamma^k_{ij} = \tfrac12 g^{kl}(\partial_i g_{jl}+\partial_j g_{il}-\partial_l g_{ij}) are the Christoffel symbols encoding intrinsic curvature.

10.2 Information Geometry and FisherRao Metric

The statistical manifold \mathcal{M} = \{p(\cdot;\theta)\} carries the FisherRao metric g_{ij}(\theta) = \mathcal{I}(\theta)_{ij}.

Natural gradient (Amari 1998): Steepest descent on (\mathcal{M}, g):

\theta \leftarrow \theta - \eta\,\mathcal{I}(\theta)^{-1}\nabla_\theta\mathcal{L}.

This is invariant to reparametrisation and achieves quadratic convergence on convex objectives — equivalent to Fisher scoring.

KL geometry: D_{\mathrm{KL}}(p_\theta\,\|\,p_{\theta+d\theta}) = \tfrac12\,d\theta^\top\mathcal{I}(\theta)\,d\theta + O(\|d\theta\|^3), confirming FisherRao as the intrinsic KL metric.

Dually flat structure: Exponential families p(x;\theta)=h(x)\exp(\theta^\top T(x)-A(\theta)) are $e$-flat in natural parameters and $m$-flat in mean parameters \eta=\nabla A(\theta), with vanishing sectional curvature K=0 — explaining exact Newton/natural-gradient convergence on these models.

10.3 Lie Groups and Geometric Control

::::{admonition} Definition — Lie Group :class: definition

A Lie group G is a smooth manifold with a group structure where multiplication and inversion are smooth. The Lie algebra \mathfrak{g} = T_e G linearises the group at the identity. ::::

Examples:

  • SO(d) — rotation group; portfolio factor rotation and orthogonality constraints.
  • Heisenberg group — path-signature feature maps (used in lab_signature_methods).

Left-invariant control system on G:

\dot g(t) = g(t)\,\xi(t), \quad g\in G,\; \xi(t)\in\mathfrak{g}.

PMP on Lie groups yields the LiePoisson (EulerPoincaré) equations (HolmMarsdenRatiu), providing structure-preserving optimal trajectories.

10.4 Symplectic Geometry and Hamiltonian Structure

The phase space (T^\star M, \omega) carries the symplectic 2-form \omega = \sum_i dp_i \wedge dq_i. Hamilton's equations preserve \omega (Liouville's theorem — phase-space volume conserved).

Connection to PMP: The costate pair (X_t^\star, p_t) solves Hamilton's equations, i.e., the PMP is a symplectic flow on T^\star\mathbb{R}^d.

Symplectic integrators (StörmerVerlet, RuthForest) preserve \omega discretely, keeping the Hamiltonian nearly constant over long horizons — critical for multi-year allocation back-tests in Optimiz-rs.

10.5 Sectional Curvature and Landscape Geometry

The sectional curvature K(\sigma) governs how quickly nearby geodesics diverge:

K > 0 (sphere): geodesics converge   -> compact optimiser trajectories
K = 0 (flat  ): Euclidean behaviour  -> Newton / natural gradient exact
K < 0 (hyper.): exponential spread   -> efficient landscape exploration

For exponential families in natural/mean parameters K=0 — explaining exact Newton convergence without curvature correction.


Quick Reference

Concept Key equation / object Optimiz-rs module
Brownian motion W_t - W_s \sim \mathcal{N}(0,t-s) point_processes
Itô SDE dX=b\,dt+\sigma\,dW ou_estimator
Poisson / Compound Poisson N_t\sim\text{Poisson}(\lambda t) point_processes
Lévy process triplet (b,\sigma^2,\nu) point_processes
HJB PDE -\partial_t V = \inf_u[\ell + \nabla V^\top b + \tfrac12\operatorname{Tr}\sigma\sigma^\top\nabla^2 V] optimal_control
HJBI (jumps) +\int[V(\cdot+c)-V-\nabla V^\top c]\nu\,dz optimal_control
PMP costate \dot p = -\nabla_x\mathcal{H}, u^\star=\arg\min_u\mathcal{H} optimal_control
MFG (HJB + KFP) fixed-point u,m mean_field_games
Kalman filter K_t = P^-H^\top(HP^-H^\top+R)^{-1} optimal_control
MALA x'=x-\tfrac{h^2}{2}\nabla U+h\xi mcmc
HMM BaumWelch EM + Viterbi hmm
Fisher information \mathcal{I}_{ij}=\mathbb{E}[\partial_i\ell\,\partial_j\ell] hmm, sparse
Natural gradient \mathcal{I}^{-1}\nabla_\theta\mathcal{L} differential_evolution
Riemannian / Lie geometry Christoffel symbols, LiePoisson equations experimental
DE (jDE) mutation + crossover + selection differential_evolution

References

  1. Øksendal, B. Stochastic Differential Equations, 6th ed. Springer, 2003.
  2. Cont, R. & Tankov, P. Financial Modelling with Jump Processes. CRC Press, 2004.
  3. Fleming, W.H. & Soner, H.M. Controlled Markov Processes and Viscosity Solutions. Springer, 2006.
  4. Lasry, J.-M. & Lions, P.-L. "Mean field games." Jpn. J. Math. 2 (2007) 229260.
  5. Amari, S. Information Geometry and Its Applications. Springer, 2016.
  6. do Carmo, M.P. Riemannian Geometry. Birkhäuser, 1992.
  7. Holm, D.D., Marsden, J.E. & Ratiu, T.S. "The EulerPoincaré equations." Adv. Math. 137 (1998).
  8. Price, K.V., Storn, R.M. & Lampinen, J.A. Differential Evolution. Springer, 2005.
  9. Roberts, G.O., Gelman, A. & Gilks, W.R. "Weak convergence of Metropolis algorithms." (1997).
  10. Merton, R.C. "Option pricing when underlying stock returns are discontinuous." JFE 3 (1976).
  11. Crandall, M.G. & Lions, P.-L. "Viscosity solutions of HamiltonJacobi equations." Trans. AMS (1983).