Uniform residual bounds for the actual coefficient field.
theorem
PlanarMidpoint.approx_actual_residual_bound
(C : E → Coeff)
(p : E)
(c : Coeff)
(J : E →L[ℝ] Coeff)
(H : Hessian)
(h : E)
(η B T ε t : ℝ)
(hη : 0 ≤ η)
(hB : 0 ≤ B)
(hε : 0 ≤ ε)
(hd : ‖approxDisplacement c J H h ε t‖ ≤ B * ε)
(hv : ‖approxVelocity c J H h ε t‖ ≤ B * ε)
(htail : ‖approxResidualTail c J H h ε t‖ ≤ T)
(hcoeff :
have d := approxDisplacement c J H h ε t;
‖C (p + d) - c - J d - (1 / 2) • (H d) d‖ ≤ η * ‖d‖ ^ 2)
:
‖approxAcceleration c J H h ε t + K (C (p + approxDisplacement c J H h ε t)) (approxVelocity c J H h ε t) (approxVelocity c J H h ε t)‖ ≤ (8 * η * B ^ 4 + T * ε) * ε ^ 4
theorem
PlanarMidpoint.short_geodesic_approximation
(C : E → Coeff)
(p : E)
(c : Coeff)
(J : E →L[ℝ] Coeff)
(H : Hessian)
(h : E)
(r M L η B T ε ρ : ℝ)
(hM : 0 ≤ M)
(hL : 0 ≤ L)
(hr : 0 < r)
(hη : 0 ≤ η)
(hB : 0 ≤ B)
(hT : 0 ≤ T)
(hε : 0 ≤ ε)
(hbound : ∀ x ∈ Metric.ball p r, ‖C x‖ ≤ M)
(hLip : ∀ x ∈ Metric.ball p r, ∀ y ∈ Metric.ball p r, ‖C x - C y‖ ≤ L * ‖x - y‖)
(hsmall : 8 * L * r ^ 2 + 16 * M * r < 1 / 2)
(hcoeff : ∀ (d : E), ‖d‖ < ρ → ‖C (p + d) - c - J d - (1 / 2) • (H d) d‖ ≤ η * ‖d‖ ^ 2)
(hsize :
∀ t ∈ Set.Icc 0 1,
‖approxDisplacement c J H h ε t‖ ≤ B * ε ∧ ‖approxVelocity c J H h ε t‖ ≤ B * ε ∧ ‖approxResidualTail c J H h ε t‖ ≤ T)
(hεr : B * ε < r)
(hερ : B * ε < ρ)
(γ v : ℝ → E)
(hγ : IsShortGeodesic C 1 p r (p - (ε / 2) • h) (p + (ε / 2) • h) γ v)
:
A short actual geodesic has the quartic midpoint polynomial as a uniform approximation. All hypotheses on the approximate trajectory are explicit polynomial bounds, while the actual curve is constrained only by the ODE.
theorem
PlanarMidpoint.exists_short_geodesic_approximation
(C : E → Coeff)
(p : E)
(c : Coeff)
(J : E →L[ℝ] Coeff)
(H : Hessian)
(h : E)
(r M L : ℝ)
(hr : 0 < r)
(hM : 0 ≤ M)
(hL : 0 ≤ L)
(hbound : ∀ x ∈ Metric.ball p r, ‖C x‖ ≤ M)
(hLip : ∀ x ∈ Metric.ball p r, ∀ y ∈ Metric.ball p r, ‖C x - C y‖ ≤ L * ‖x - y‖)
(hsmall : 8 * L * r ^ 2 + 16 * M * r < 1 / 2)
(hTaylor : ∀ η > 0, ∃ ρ > 0, ∀ (d : E), ‖d‖ < ρ → ‖C (p + d) - c - J d - (1 / 2) • (H d) d‖ ≤ η * ‖d‖ ^ 2)
(κ : ℝ)
(hκ : 0 < κ)
:
Uniform fourth-order approximation, expressed without any differentiability of the endpoint-to-geodesic choice.