- Anderson's theorem
In
mathematics , Anderson's theorem is a result inreal analysis andgeometry which says that theintegral of an integrable, symmetric, unimodal, non-negative function "f" over an "n"-dimensionalconvex body "K" does not decrease if "K" is translated inwards towards the origin. This is a natural statement, since thegraph of "f" can be thought of as a hill with a single peak over the origin; however, for "n" ≥ 2, the proof is not entirely obvious, as there may be points "x" of the body "K" where the value "f"("x") is larger than at the corresponding translate of "x".Anderson's theorem also has an interesting application to
probability theory .tatement of the theorem
Let "K" be a convex body in "n"-
dimension alEuclidean space R"n" that is symmetric with respect to reflection in the origin, i.e. "K" = −"K". Let "f" : R"n" → R be a non-negative, symmetric, globally integrable function; i.e.
* "f"("x") ≥ 0 for all "x" ∈ R"n";
* "f"("x") = "f"(−"x") for all "x" ∈ R"n";
*Suppose also that the super-
level set s "L"("f", "t") of "f", defined by:
are convex subsets of R"n" for every "t" ≥ 0. (This property is sometimes referred to as being unimodal.) Then, for any 0 ≤ "c" ≤ 1 and "y" ∈ R"n",
:
Application to probability theory
Given a
probability space (Ω, Σ, Pr), suppose that "X" : Ω → R"n" is an R"n"-valuedrandom variable withprobability density function "f" : R"n" → [0, +∞) and that "Y" : Ω → R"n" is an independent random variable. The probability density functions of many well-known probability distributions are "p"-concave for some "p", and hence unimodal. If they are also symmetric (e.g. the Laplace andnormal distribution s), then Anderson's theorem applies, in which case:
for any origin-symmetric convex body "K" ⊆ R"n".
References
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