Differentiability at means that there is a linear map such that
The partial derivatives are when the derivative exists; independently, they may be defined by the corresponding one-variable difference quotients.
Suppose the partial derivatives exist near and are continuous at . Apply the one-dimensional mean value theorem along the two coordinate segments from to . It gives intermediate points such that
Continuity of the partials makes the remainder after subtracting
equal to . Hence is differentiable and this is its derivative.
For the given function, writing , at we have
At the origin both partial derivatives are zero, since and tend to zero. Neither partial is continuous there: along its corresponding coordinate axis the cosine term oscillates without a limit. Nevertheless
so is differentiable at the origin with derivative zero. This illustrates that existence of partial derivatives does not imply their continuity.
The final assertion is false. Define
Again , so is differentiable at the origin and it is smooth elsewhere. But along the -axis,
is unbounded near zero, and similarly is unbounded. Thus both partial derivatives can be unbounded in every neighbourhood of a point even when the function is differentiable everywhere.
Fix . The map is a linear functional, so the finite-dimensional Riesz representation theorem gives a unique vector such that
For scalars ,
Uniqueness gives
so is linear.
For , apply this result to
It produces a unique linear map satisfying
which proves existence and uniqueness of the adjoint.
The steady Euler equations for an inviscid fluid are
Taking the scalar product with and using
gives
Thus
The Bernoulli function is constant along each streamline: fluid particles in steady flow exchange pressure, kinetic, and potential energy without changing their total mechanical energy density.
Let be the downward displacement of the free surface from its initial level, and let be the speed in the tube. Conservation of volume gives
The free surface and the outlet are both at atmospheric pressure, and their vertical separation is . Applying the Bernoulli equation between them, while retaining the small free-surface speed, gives
Therefore
The surface reaches the upper tube end when . Hence the draining time of a uniform tank through a siphon is
Set . Periodicity and separation of variables give the angular modes , , and . The radial equation is
whose solutions are for ; the zero mode has solutions and . Thus a general real harmonic function on the annulus is
The boundary data contain only the cosine mode, so write
The condition at gives , and the condition at fixes . The Dirichlet problem on an annulus for one Fourier mode therefore has solution
For a general Lagrangian,
Along an Euler-Lagrange trajectory,
so energy is conserved when has no explicit time dependence.
For the given Lagrangian, write . At points where ,
The Euler-Lagrange equation is therefore
In expanded form its left-hand side is
The momentum has fixed magnitude,
so this is constant without needing to solve the equation of motion. The Hamiltonian is
The singular Legendre transform of a degree-one velocity Lagrangian applies here: determines only the direction of , not its magnitude, and the velocity Hessian is not invertible. Thus the usual inverse Legendre transform cannot reconstruct the Lagrangian from this Hamiltonian.
The Cauchy integral theorem states that if is holomorphic on a simply connected domain, then its integral around every closed piecewise smooth contour in that domain is zero.
Put . Completing the square gives
After the change of variable , the integral runs along the horizontal line . The integrand is entire. Apply Cauchy's theorem to a rectangle joining this line to the real axis; the two vertical integrals tend to zero as their real parts tend to , because . The contour may therefore be shifted to the real line. Hence the Fourier transform of a Gaussian gives
Use the global parametrization
Its tangent vectors are
and
Thus is a regular parametrization and the graph is a smooth surface.
The first fundamental form is
Choosing the upward orientation, the Gauss map is

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