In mathematics, the oscillation of a function or a sequence is a number that quantifies how much that sequence or function varies between its extreme values as it approaches infinity or a point. As is the case with limits, there are several definitions that put the intuitive concept into a form suitable for a mathematical treatment: oscillation of a sequence of real numbers, oscillation of a real-valued function at a point, and oscillation of a function on an interval (or open set).
Let
(an)
\omega(an)
(an)
\omega(an)=\limsupn\toinftyan-\liminfn\toinftyan
The oscillation is zero if and only if the sequence converges. It is undefined if
\limsupn\toinfty
\liminfn\toinfty
Let
f
f
I
f
\omegaf(I)=\supx\inf(x)-infx\inf(x).
f:X\toR
X
f
U
\omegaf(U)=\supx\inf(x)-infx\inf(x).
The oscillation of a function
f
x0
\epsilon\to0
f
\epsilon
x0
\omegaf(x0)=\lim\epsilon\to\omegaf(x0-\epsilon,x0+\epsilon).
x0
x0
More generally, if
f:X\toR
\omegaf(x0)=\lim\epsilon\to\omegaf(B\epsilon(x0)).
1 | |
x |
x
x
\sin
1 | |
x |
x
\sinx
x
(-1)x
In the last example the sequence is periodic, and any sequence that is periodic without being constant will have non-zero oscillation. However, non-zero oscillation does not usually indicate periodicity.
Geometrically, the graph of an oscillating function on the real numbers follows some path in the xy-plane, without settling into ever-smaller regions. In well-behaved cases the path might look like a loop coming back on itself, that is, periodic behaviour; in the worst cases quite irregular movement covering a whole region.
Oscillation can be used to define continuity of a function, and is easily equivalent to the usual ε-δ definition (in the case of functions defined everywhere on the real line): a function ƒ is continuous at a point x0 if and only if the oscillation is zero;[1] in symbols,
\omegaf(x0)=0.
For example, in the classification of discontinuities:
This definition is useful in descriptive set theory to study the set of discontinuities and continuous points – the continuous points are the intersection of the sets where the oscillation is less than ε (hence a Gδ set) – and gives a very quick proof of one direction of the Lebesgue integrability condition.[2]
The oscillation is equivalent to the ε-δ definition by a simple re-arrangement, and by using a limit (lim sup, lim inf) to define oscillation: if (at a given point) for a given ε0 there is no δ that satisfies the ε-δ definition, then the oscillation is at least ε0, and conversely if for every ε there is a desired δ, the oscillation is 0. The oscillation definition can be naturally generalized to maps from a topological space to a metric space.
More generally, if f : X → Y is a function from a topological space X into a metric space Y, then the oscillation of f is defined at each x ∈ X by
\omega(x)=inf\left\{diam(f(U))\midU is a neighborhood of x\right\}