The eikonal equation in is given by
.
In his first lecture, Arnold mentioned that the solutions to the above equation are functions that are (at least locally) the sum of a constant and the distance to some curve.
Given the initial value problem:
,
the unique solution would be the distance of each point to the curve .
Let’s take a look at a few examples.
Example 1: Let be the unit square centered at the origin in
. Consider the IVP
where
The graph of the unique solution defined on the domain inside is the square-based pyramid with height 1/2:

Notice, the solution is not smooth along the diagonals of the square. The projection of the characteristic field onto the (x,y)-plane is just the field of vectors such that the length of the vector at each point is the distance from the point to the square and the direction of each vector is along the line of shortest distance from the point to the square.
Similarly, if we use the unit circle as the zero set for in the initial value problem, the graph solution defined on the unit disk would be the cone centered at the origin of height 1/2. The unique solution is given by $latex u(x, y) = |\sqrt{x^2 + y^2} – 1|.
Let’s now derive this using the characteristic vector field.
describes a surface in
.
Let ,
. The coordinates in
are given by
.
If we write the PDE as a Hamilton-Jacobi equation, we have:
(the 1/2 coefficient at the front does not affect the solutions; it is simply used to make the computations later slightly more simple)
From lecture 2 of Arnold’s PDE, the characteristic vector field is given by:
Since , it follows that $p_x, p_y$ are constants, say
, along each characteristic (i.e. each phase curve of the characteristic vector field).
Hence, the projection of each characteristic onto the (x,y)-plane is:
, where
are initial values at t = 0.
Since , it follows that
, where
is the initial value at t = 0.
Goal: find the value of for each characteristic.
Parameterizing the unit circle by :
We also want .
Key: is the gradient of
at
. We now know that a level curve of
is given by the unit circle
. The gradient is orthogonal to the tangent of the level curve. Thus at
, the corresponding
must be a multiple of the normal vector of the unit circle
. Since
,
.
Hence, for a characteristic corresponding to parameter s, we have:
(when t = 0, we are on the unit circle)
Notice that .
It follows that , which is what we want.
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