The coordinate curves are assumed to be geodesics as geometric curves; use their arc-length parametrization in the geodesic equations. On , choose increasing arc length , so and . The transverse equation becomes
Thus . On , similarly , , and the transverse equation gives . Hence the geodesic coordinate grid identities are
For , use the Bromwich inversion formula with a vertical contour :
Close the contour to the left, where the exponential decays. The large-arc contribution tends to zero by the usual exponential arc estimate, and the two simple poles are at and . The residues of the complete integrand are and . The residue theorem therefore gives
The right limit at zero is one. The sign of nonzero real has no effect on the answer.
The set is a rational comb with a connecting spine: it contains the whole vertical segment , and every horizontal segment at rational height. Any point with has rational height and can move horizontally to the vertical segment without leaving the set. It can then move vertically to . Points already on the vertical segment use only the second step. Concatenating these polygonal paths connects any two points. Consequently
No claim about a horizontal segment at irrational height is needed: at such a height, the only point in the set lies on the connecting spine.
Use the continuous slope map on the given set, where . The attained ratios are positive rational numbers. Choosing the irrational cut , the two subsets
are disjoint, relatively open, and cover the entire set. Both are nonempty: ratios one and two are attained inside the square. This irrational-cut separation of rational slopes is a separation, so
The individual rational-slope rays are connected, but their common origin is excluded; their separate connectivity does not imply connectivity of their union.
Substitute the rotating velocity field into the Euler equations for an inviscid fluid. Its acceleration is , so
The preceding angular acceleration makes both mixed coefficients , ensuring integrability. Thus
Pressure is determined up to the spatially uniform function . The specified force has no vertical component; if gravity were additionally included in the body force, the usual hydrostatic term would also appear. It is not implied by the displayed force here.
The Euler equations for an inviscid fluid are . Here the vorticity is , and direct differentiation gives , whose curl vanishes. Taking the curl therefore gives
so
For constant force coefficients and the initial rest condition, . Only the antisymmetric part of the horizontal force gradient generates rotation; its symmetric part is balanced by pressure.
At height , . Integrating over a circular cross-section cancels the horizontal components by symmetry. Thus the angular momentum per unit length is
The coefficient is the polar moment of inertia per unit length of the liquid column.
The rigid-rotation velocity field is , with spatially uniform . Its divergence is zero, since . It therefore satisfies the incompressible continuity equation. On the cylindrical wall, , so it has zero normal velocity; on either end cap its vertical component is zero. These are the impermeability boundary conditions for an inviscid flow. Tangential slip is permitted; a no-slip condition is not part of this inviscid model.
Use real physical fields in the quadratic energy expressions. The vector identity and vacuum Maxwell's equations give
Integrating over a fixed volume and applying the divergence theorem proves Poynting's theorem:
The left side is outward energy flux through the closed surface, not merely local intensity.
For a linearly polarized wave with phase , the real fields give Poynting vector . Local intensity oscillates at . In the closed-surface integral, the time-independent part cancels because . The remaining flux generally oscillates at , has zero time average, and may vanish identically for special volume geometries.
For circular polarization, take with orthonormal transverse vectors. Then and , so is spatially and temporally constant. Therefore the closed-surface Poynting flux of a plane wave is
There is still a nonzero steady local energy flow: equal energy enters and leaves every fixed closed volume. Calling the net closed-surface flux a nonzero constant would confuse these two quantities.
Vacuum Maxwell's equations are invariant under spatial rotations. Rotate the preceding coordinate system so that becomes the propagation direction , and rotate the transverse electric direction to a unit polarization vector . Dot and cross products transform covariantly under this rotation, so transversality and the field relation are unchanged. With ,
These complex fields encode real fields through their real parts. The displayed form describes linear electromagnetic polarization; a general transverse complex amplitude can describe elliptical or circular electromagnetic polarization as well.
For these plane waves, the vacuum Faraday law reads
Cancel the nonzero factor to obtain
For positive-frequency propagation in the positive direction, .
Substitute the monochromatic plane waves into the two divergence equations of Maxwell's equations. They become and . For nonzero wavenumber,
Thus both fields are transverse to the direction of propagation. The wave equation also gives the vacuum dispersion relation .
Take the curl of the vacuum Faraday law and use the vacuum Ampere-Maxwell law:
Since the electric divergence vanishes, the double-curl identity makes the left side . Therefore the electromagnetic wave equation is
The same calculation interchanging the fields gives the wave equation for .
Suppose an open hyperbolic disc centred at is contained in a hyperbolic triangle. Move to zero by an isometry. Extend the radial geodesics from zero through the three vertices to ideal points . Because zero lies inside the original triangle, the three vertex directions are not contained in a semicircle. The ideal hyperbolic triangle with those endpoints therefore contains zero: otherwise a separating geodesic through zero would put all three endpoints in one semicircle. It also contains each finite vertex, which lies on the segment from zero to the corresponding ideal endpoint. Geodesic convexity then makes it contain the original triangle.
The three angular gaps between successive ideal endpoints sum to , and each is at most . One has size at least , so its half-angle is at least . The distance in part (iii) decreases as increases. Thus the corresponding side of the ideal triangle is at distance at most
from zero. If the disc radius exceeds this distance, it contains a point on that side and points beyond it, and cannot be contained in the ideal triangle, hence cannot be contained in the original one. This proves the hyperbolic triangle inradius bound:
The symmetric ideal triangle has equality, explaining the constant. Finite triangles have strictly smaller inradius.
Rotate the disc so that and , with representing half the smaller angle. For , the hyperbolic line joining them is the arc of a circle orthogonal to the unit circle. Its Euclidean centre is real, say , and orthogonality gives squared radius . Substituting into gives , with radius .
The arc's point nearest zero is on the positive real axis, at
Distance from zero in the Poincare disc model increases with Euclidean modulus, by the radial-length calculation. Therefore
For , the hyperbolic line is a diameter through zero and its distance is zero, agreeing with the continuous limit of the formula. Choosing the smaller endpoint angle avoids a spurious negative value caused by an inappropriate oriented-angle convention.
For the Poincare disc model, radial distance from zero to Euclidean radius is
It is minimal: any curve has length at least the integral of , which in turn is at least the net radial integral. Consequently a hyperbolic circle of radius centred at zero is , a Euclidean circle.
Given a centre , use a Poincare disc automorphism carrying to zero. Since it is an isometry, it takes the given hyperbolic circle to the preceding Euclidean circle. A Möbius transformation takes generalized circles to generalized circles. The preimage here is compact and contained in the disc, so it cannot be a straight line. Thus
This argument does not say that their Euclidean and hyperbolic centres coincide.
For , let . Direct calculation gives
Its denominator does not vanish in the disc, and this identity shows that it maps the disc into itself. Its inverse has the same property, so is a Poincare disc automorphism. Multiplication by a complex number of modulus one is another such automorphism.
Conversely let be a Möbius transformation mapping the disc onto itself, and let . Then is a disc automorphism fixing zero, say with . Since it maps the boundary circle to itself, for every . This forces , hence and . Thus is a rotation , and . Absorb the denominator's minus sign into to obtain precisely the paper's convention:
Here mapping the disc to itself means bijectively onto itself; there are nonautomorphic Möbius transformations whose image is a proper subdisc.
Because the velocity is independent of , the vortex-stretching term is . Substituting , and into the vorticity equation and cancelling a minus sign gives
The planar vorticity is transported by the flow without vortex stretching under these inviscid assumptions.
For the stated incompressible planar flow, use the stream function convention , . It gives and the vorticity is
Thus , where the Laplacian is the two-dimensional one.
The first column already has zeros below the top entry. In the last three rows of the second column, reflect to using . Since , the Householder reflection is
With , direct multiplication gives
The transformed least-squares objective is . Its first two squares can both vanish, so the unique answer is
Uniqueness follows because the triangular leading block is invertible; this calculation implements Householder QR decomposition without squaring the condition number through normal equations.

There are unlisted articles, also show them or only show them.