Physical covariance of the actual wave curl #
The potential is differentiated before any cutoff or carrier is removed. All operators below are actual Frechet derivatives.
Cylinder: an abbreviation for PhysicalResidualBridge.Cylinder.
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Scaled graph: an abbreviation for PhysicalResidualBridge.ScaledGraph.
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Real vector, given by AxisymmetricResidual.pack (a 0).re (a 1).re (a 2).re.
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- NavierStokes.PhysicalCurlCovariance.realVector a = NavierStokes.AxisymmetricResidual.pack (a 0).re (a 1).re (a 2).re
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Real curl as an element of Fin 3 → ℝ.
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Curl, like its underlying alternating tensor, rotates with an oriented orthonormal cylindrical frame.
Cylindrical spatial curl, constructed using AxisymmetricResidual.pack.
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The moving-frame connection term is part of the genuine Cartesian curl.
The phase rescaling and inverse carrier cancel exactly. This is why the potential has one fewer inverse length than the velocity.
A potential value identity gives its physical curl identity by the actual chain rule. It is not necessary to assume matching velocity fields.
Complex potential, given by (c : ℂ) • B (G.map z).
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- G.complexPotential c B z = ↑c • B (NavierStokes.PhysicalResidualBridge.ScaledGraph.map G z)
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Real potential, defined pointwise by realVector (complexPotential G c B z).
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- G.realPotential c B z = NavierStokes.PhysicalCurlCovariance.realVector (G.complexPotential c B z)
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Coordinate reassociation and smooth cutoffs.
Reindex vector, given by e.symm (V (e x)).
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- NavierStokes.PhysicalCurlCovariance.reindexVector e V x = e.symm (V (e x))
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Cutoff differentiation produces the full gradient-cross-potential term.
A local equality of the full potentials, including their cutoffs and carriers, automatically propagates to equality of actual curls.
Radial curve, given by ((1, ((0, 0), (G.frequency * GraphCalculus.radialSpeed G.exponent r) • G.radialVector)), 0).
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Arbitrary native or common covering index, with the exact potential
weight Q^(-h) and velocity weight Q^(-A).
Derivation of the potential pullback from raw amplitude and phase
scaling. The real factor b also covers signed harmonics.
The single reference potential expressed in physical cylindrical coordinates, before taking its real part and rotating to Cartesian axes.
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Potential covariance is derived from the primitive phase and amplitude identities. No identity between curls or corrected velocities is assumed.
One Cartesian reference potential supplies every compatible band's actual corrected wave. Amplitude and phase compatibility are primitive field-value identities; the curl and cutoff derivatives are derived.
The coefficient used by the wave pipeline, after the cutoff, is the coefficient of the actual curl. The cutoff is applied exactly once.
Annularly localized potentials have zero actual curl on the axis, without assigning a cylindrical angle there.
A concrete Cartesian potential in an actual inverse polar chart #
Polar input, given by PolarCharts.chart a j (PhysicalGraphBounds.radialProjection z).
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Polar coordinates, given by (z.1, AxisymmetricResidual.pack (polarInput a j z).1 (polarInput a j z).2 (z.2 2)).
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The actual Cartesian field, not a prescribed derivative or a matching predicate. Its inverse polar chart has a smooth global extension.
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Valid cylindrical as an element of Set SpaceTime.
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The constructed Cartesian potential has the prescribed actual curl in its polar chart. No potential-representation premise remains.
Periodicity of the full cylindrical potential gives equality of the constructed Cartesian potentials on chart overlaps.
A single actual Cartesian potential is selected from the compatible local inverse charts. Outside their union it is defined to be zero.
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Annular vanishing removes the boundary of the selected-chart union; the resulting Cartesian potential is genuinely smooth everywhere.
The potential need only be smooth on the physical time domain; no extension through a possible singular terminal time is required.
Cartesian velocity, given by SpatialCurl.spatialCurl (globalCartesianPotential a B).
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Integer angular frequency makes the complete potential periodic, including its normal coefficient and inverse carrier.
The end-to-end band reconstruction uses a single explicitly constructed Cartesian potential. Only primitive phase/amplitude compatibility and periodicity are inputs; potential and curl compatibility are conclusions.