Level set

Points at constant slices of x₂ = f (x₁).

Lines at constant slices of x₃ = f (x₁, x₂).

Planes at constant slices of x₄ = f (x₁, x₂, x₃).

(n − 1)-dimensional level sets for functions of the form f (x₁, x₂, …, x_n) = a₁x₁ + a₂x₂ + ⋯ + a_nx_n where a₁, a₂, …, a_n are constants, in (n + 1)-dimensional Euclidean space, for n = 1, 2, 3.

Points at constant slices of x₂ = f (x₁).

Contour curves at constant slices of x₃ = f (x₁, x₂).

Curved surfaces at constant slices of x₄ = f (x₁, x₂, x₃).

(n − 1)-dimensional level sets of non-linear functions f (x₁, x₂, …, x_n) in (n + 1)-dimensional Euclidean space, for n = 1, 2, 3.

In mathematics, a level set of a real-valued function f of n real variables is a set where the function takes on a given constant value c, that is:

L c ( f ) = { ( x 1 , … , x n ) ∣ f ( x 1 , … , x n ) = c }   . {\displaystyle L_{c}(f)=\left\{(x_{1},\ldots ,x_{n})\mid f(x_{1},\ldots ,x_{n})=c\right\}~.}

When the number of independent variables is two, a level set is called a level curve, also known as contour line or isoline; so a level curve is the set of all real-valued solutions of an equation in two variables x₁ and x₂. When n = 3, a level set is called a level surface (or isosurface); so a level surface is the set of all real-valued roots of an equation in three variables x₁, x₂ and x₃. For higher values of n, the level set is a level hypersurface, the set of all real-valued roots of an equation in n > 3 variables (a higher-dimensional hypersurface).

A level set is a special case of a fiber.

Level sets show up in many applications, often under different names. For example, an implicit curve is a level curve, which is considered independently of its neighbor curves, emphasizing that such a curve is defined by an implicit equation. Analogously, a level surface is sometimes called an implicit surface or an isosurface.

The name isocontour is also used, which means a contour of equal height. In various application areas, isocontours have received specific names, which indicate often the nature of the values of the considered function, such as isobar, isotherm, isogon, isochrone, isoquant and indifference curve.

Consider the 2-dimensional Euclidean distance: d ( x , y ) = x 2 + y 2 {\displaystyle d(x,y)={\sqrt {x^{2}+y^{2}}}} A level set L r ( d ) {\displaystyle L_{r}(d)} of this function consists of those points that lie at a distance of r {\displaystyle r} from the origin, that make a circle. For example, ( 3 , 4 ) ∈ L 5 ( d ) {\displaystyle (3,4)\in L_{5}(d)} , because d ( 3 , 4 ) = 5 {\displaystyle d(3,4)=5} . Geometrically, this means that the point ( 3 , 4 ) {\displaystyle (3,4)} lies on the circle of radius 5 centered at the origin. More generally, a sphere in a metric space ( M , m ) {\displaystyle (M,m)} with radius r {\displaystyle r} centered at x ∈ M {\displaystyle x\in M} can be defined as the level set L r ( y ↦ m ( x , y ) ) {\displaystyle L_{r}(y\mapsto m(x,y))} .

A second example is the plot of Himmelblau's function shown in the figure to the right. Each curve shown is a level curve of the function, and they are spaced logarithmically: if a curve represents L x {\displaystyle L_{x}} , the curve directly "within" represents L x / 10 {\displaystyle L_{x/10}} , and the curve directly "outside" represents L 10 x {\displaystyle L_{10x}} .

Theorem: If the function f is differentiable, the gradient of f at a point is either zero, or perpendicular to the level set of f at that point.

To understand what this means, imagine that two hikers are at the same location on a mountain. One of them is bold, and decides to go in the direction where the slope is steepest. The other one is more cautious and does not want to either climb or descend, choosing a path which stays at the same height. In our analogy, the above theorem says that the two hikers will depart in directions perpendicular to each other.

A consequence of this theorem (and its proof) is that if f is differentiable, a level set is a hypersurface and a manifold outside the critical points of f. At a critical point, a level set may be reduced to a point (for example at a local extremum of f ) or may have a singularity such as a self-intersection point or a cusp.

A set of the form

L c − ( f ) = { ( x 1 , … , x n ) ∣ f ( x 1 , … , x n ) ≤ c } {\displaystyle L_{c}^{-}(f)=\left\{(x_{1},\dots ,x_{n})\mid f(x_{1},\dots ,x_{n})\leq c\right\}}

is called a sublevel set of f (or, alternatively, a lower level set or trench of f). A strict sublevel set of f is

{ ( x 1 , … , x n ) ∣ f ( x 1 , … , x n ) < c } {\displaystyle \left\{(x_{1},\dots ,x_{n})\mid f(x_{1},\dots ,x_{n})<c\right\}}

Similarly

L c + ( f ) = { ( x 1 , … , x n ) ∣ f ( x 1 , … , x n ) ≥ c } {\displaystyle L_{c}^{+}(f)=\left\{(x_{1},\dots ,x_{n})\mid f(x_{1},\dots ,x_{n})\geq c\right\}}

is called a superlevel set of f (or, alternatively, an upper level set of f). And a strict superlevel set of f is

{ ( x 1 , … , x n ) ∣ f ( x 1 , … , x n ) > c } {\displaystyle \left\{(x_{1},\dots ,x_{n})\mid f(x_{1},\dots ,x_{n})>c\right\}}

Sublevel sets are important in minimization theory. By Weierstrass's theorem, the boundness of some non-empty sublevel set and the lower-semicontinuity of the function implies that a function attains its minimum. The convexity of all the sublevel sets characterizes quasiconvex functions.^[2]

• Epigraph
• Level-set method
• Level set (data structures)