For a steady flow independent of , geostrophic balance gives
Hence , and the definition of becomes
Equivalently,
With the Rossby deformation radius , the bounded solution for the stated potential-vorticity step is
Continuity of and at gives
Therefore
and
When , the surface height increases smoothly from to , while is a positive eastward jet with its maximum at the discontinuity and exponential decay on the Rossby-radius scale:
The vertical relative vorticity is
Differentiate the -momentum equation with respect to and the -momentum equation with respect to , then subtract. The mixed pressure derivatives cancel, giving
The mass-conservation equation says . Therefore the linearized shallow-water potential vorticity
satisfies
Thus
The constant is the positive Coriolis parameter at northern latitude , is the gravitational acceleration, and is the undisturbed mean depth of the layer.
The linearized shallow water equations assume a homogeneous, incompressible, inviscid layer over a flat bed; a horizontal scale much larger than the depth, so the shallow-water approximation and hydrostatic approximation apply; depth-independent horizontal velocity; a free-surface displacement and sufficiently small velocity to neglect nonlinear products; and an f-plane on which is constant. The equations also omit viscosity, forcing, and bottom topography.
For and , the linear ordinary differential equation is , whose general solution is
By the stated parity reduction, an even eigenfunction has the form . The conditions have a nonzero solution exactly when
that is,
An odd eigenfunction has the form , and the corresponding determinant gives
Thus is an eigenvalue precisely under one of the two stated conditions.
Figure 1.
The fourth-order eigenvalue condition and its roots
. Details.
For the minus sign, division by away from gives . On , for , while on their signs differ, so there is no root. For the plus sign the equation is
There is no root in . On , the function increases strictly from to , so it has exactly one root by the intermediate value theorem. Numerically,
Hence the combined condition has exactly one solution in .
With and , the equation is
Multiply by the real eigenfunction and integrate over . The clamped boundary conditions at both endpoints eliminate all boundary terms, so
Since , the right side is a sum of nonnegative terms. It cannot vanish for a nonzero eigenfunction: if , the boundary conditions force . Thus
Let . Repeated integration by parts gives the formal adjoint rules
Therefore
Equality of the coefficients of in and requires
so . This also makes the zeroth-order coefficients equal because . Hence, under boundary conditions that remove the boundary terms,
This is the self-adjoint fourth-order scalar differential operator .
For , completing the square gives the Bogomolny bound
Consequently
with equality exactly when the Bogomolny equation
holds everywhere. Separating variables, or differentiating the proposed form directly, gives all solutions with the required limits:
These are the translated phi-four kinks.
Differentiating the first-order equation yields
which is precisely the Euler-Lagrange equation from part (a). Thus every configuration saturating the first-order bound is automatically a stationary solution of the second-order variational equation.
The integrand
is nonnegative, so . If , both continuous summands vanish everywhere. Hence , so is constant; the common boundary value forces . Conversely, has and , so . Therefore
This agrees with part (a): at , the first variation vanishes because , and
Thus the constant configuration is a stationary local minimum as well as the global minimum identified directly.
Write the admissible variation as , where at both ends. Differentiating the functional under the integral sign gives the first variation
After integration by parts, with the boundary term vanishing,
Thus the Euler-Lagrange equation is
A second differentiation gives the second variation
Yes. By an element of , part (a) puts the side between the - and -vertices on and the first vertex at . A reflection if needed puts the triangle on the chosen side. The remaining freedom is the ratio of the heights of the second and first vertices, and the equation from part (c) determines it uniquely because is strictly increasing on . The two incident circles are then fixed, so their other intersection and the triangle are fixed. Thus triangles with the same three angles are isometric, which is Hyperbolic AAA congruence.
Because the half-plane metric is a conformal rescaling of the Euclidean metric, its angles are Euclidean angles. For each , the hyperbolic lines meeting the imaginary axis at a fixed angle at are the Euclidean circles
where denotes the vertical coordinate. These circles have centres on the real axis and are therefore hyperbolic lines; varying gives the required collection.
To construct a triangle, put one vertex at and a second at on , with . Draw from these vertices the lines making interior angles and with . Their Euclidean centres and radii are
If their other intersection has angle , the law of cosines in the Euclidean triangle formed by the two centres and that intersection gives
Equivalently,
The right side is greater than one exactly when . Since ranges continuously and strictly increasingly from to infinity for , such a exists. The three lines therefore bound a hyperbolic triangle with the prescribed angles.
An orientation-preserving isometry fixing every point of fixes more than two points in the upper half-plane and hence, as a Möbius transformation, is the identity. The map
fixes pointwise and preserves the hyperbolic metric; it is the hyperbolic reflection in . Consequently the pointwise stabilizer is exactly
For any isometry , use part (a) to choose that agrees with on one pointed line and its tangent direction. Then fixes that line pointwise, so it is either the identity or its reflection. Hence the Isometry group of the Poincare half-plane consists of
and
with real coefficients, modulo multiplication of all four coefficients by a nonzero scalar.
A Geodesic in the Poincare half-plane model is a vertical line or a semicircle orthogonal to the real axis. Given a hyperbolic line , choose a real Möbius transformation sending its two ideal endpoints to and . After multiplying its representing matrix by a scalar and, if necessary, changing its sign, it represents an element of and sends to the positive imaginary axis .
The chosen point then maps to for some . The dilation , represented by
fixes and sends to . Thus every pointed line can be sent to , proving transitivity on pointed hyperbolic lines.
Taking and using gives
Set . The Taylor series of the denominator is
Consequently
The singular part at is therefore
Using long-time asymptotics from a Laplace transform and part (a), the centre temperature has late-time behaviour
Taking the Laplace transform in and using the initial condition , the radial heat equation in three dimensions becomes
Put and . Then
so
Finiteness at the centre forces .
The transformed boundary condition is
Since
substitution and cancellation of the two terms gives
Hence
and the required explicit transform is
The Bromwich inversion formula gives
For , close the Bromwich contour in the left half-plane. The only enclosed singularity is the double pole at , whose residue is
The residue theorem therefore yields
Define a continuous map by the standard embedded torus of revolution parametrization
Its image lies in because
The periodicity of the trigonometric functions makes and , so is constant on every -equivalence class. The universal property of the quotient topology therefore gives a unique continuous map
Every point of has cylindrical radius between and , so its polar angle determines modulo one, while the pair on the unit circle determines modulo one. Hence is surjective, and two parameters have the same image exactly when they differ by the endpoint identifications defining ; thus it is injective.
The quotient is compact as the continuous image of the given compact space under the quotient map. The surface is Hausdorff because it has the subspace topology inherited from . The compact-to-Hausdorff continuous bijection theorem now shows that is a homeomorphism. Therefore
A closed set is compact because it is closed in the compact space . Its image is compact by the fact that a continuous image of a compact space is compact, and every compact subset of the Hausdorff space is closed. Thus the continuous bijection is a closed map. Its inverse is consequently continuous, so is a homeomorphism. This is the compact-to-Hausdorff continuous bijection theorem.
If , the subspace topology on is
If is an equivalence relation on and is the natural projection, the quotient topology declares open exactly when is open in . For topological spaces and , the product topology on has as a basis all sets with open in and open in .

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