The forced initial value problem from a homogeneous evolution #
The source assumes a bound for the homogeneous tangent propagator. Here a homogeneous fundamental evolution is the input; the forced path is an actual Bochner integral. Its differential equation, initial trace, uniqueness, and weighted bounds are proved, rather than included in the evolution data.
A homogeneous fundamental evolution, with its actual inverse. This data contains no forced solution or estimate for one.
Forward of
Evolution, of typeC(Icc (0 : ℝ) T,E →L[ℝ] E).Backward of
Evolution, of typeC(Icc (0 : ℝ) T,E →L[ℝ] E).- derivative (t : ↑(Set.Icc 0 T)) : HasDerivWithinAt (EulerVolterraConvolution.extendPath T hT self.forward) (B t ∘SL self.forward t) (Set.Icc 0 T) ↑t
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The inverse fundamental map's derivative follows from the inverse theorem.
The two-time homogeneous propagator.
Equations
- U.propagator t s = U.forward t ∘SL U.backward s
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The forcing pulled back by the inverse homogeneous evolution.
Equations
- U.transformedForcing f s = (EulerVolterraConvolution.extendPath T hT U.backward s) (EulerVolterraConvolution.extendPath T hT f s)
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The pulled-back forcing is genuinely continuous.
Duhamel's formula, as an actual interval integral.
Equations
- U.solutionReal f a₀ t = (EulerVolterraConvolution.extendPath T hT U.forward t) ((U.backward ⟨0, ⋯⟩) a₀ + ∫ (s : ℝ) in 0..t, U.transformedForcing f s)
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The constructed forced path is continuous.
The actual continuous forced solution on the time interval.
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Duhamel's formula attains the prescribed initial data.
The actual constructed path solves the inhomogeneous differential equation.
The same solution has the literal two-time Duhamel formula.
Any differentiable path with the same forcing and initial data equals the actual integral construction. No uniqueness assertion is assumed of the data.
A relative homogeneous propagator bound yields the forced bound with the same profile. No exponential in the coefficient norm is introduced.