Ambit field

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In mathematics, an ambit field is a d-dimensional random field describing the stochastic properties of a given system. The input is in general a d-dimensional vector (e.g. d-dimensional space or (1-dimensional) time and (d − 1)-dimensional space) assigning a real value to each of the points in the field. In its most general form, the ambit field, Y, is defined by a constant plus a stochastic integral, where the integration is done with respect to a Lévy basis, plus a smooth term given by an ordinary Lebesgue integral. The integrations are done over so-called ambit sets, which is used to model the sphere of influence (hence the name, ambit, Latin for "sphere of influence" or "boundary") which affect a given point.

The use and development of ambit fields is motivated by the need of flexible stochastic models to describe turbulence[1] and the evolution of electricity prices[2] for use in e.g. risk management and derivative pricing. It was pioneered by Ole E. Barndorff-Nielsen and Jürgen Schmiegel to model turbulence and tumour growth.[1]

Note, that this article will use notation that includes time as a dimension, i.e. we consider (d − 1)-dimensional space together with 1-dimensional time. The theory and notation easily carries over to d-dimensional space (either including time herin or in a setting involving no time at all).

Intuition and motivation

In stochastic analysis, the usual way to model a random process, or field, is done by specifying the dynamics of the process through a stochastic (partial) differential equation (SPDE). It is known, that solutions of (partial) differential equations can in some cases be given as an integral of a Green's function convolved with another function – if the differential equation is stochastic, i.e. contaminated by random noise (e.g. white noise) the corresponding solution would be a stochastic integral of the Green's function. This fact motivates the reason for modelling the field of interest directly through a stochastic integral, taking a similar form as a solution through a Green's Function, instead of first specifying a SPDE and then trying to find a solution to this. This provides a very flexible and general framework for modelling a variety of phenomena.[2]

Definition

A tempo-spatial ambit field, Y, is a random field in space-time χ×ℝ taking values in ℝ. Let μ∈ℝ,At(x),Bt(x) be ambit sets in χ×ℝ+,g,q deterministic kernel functions, a a stochastic function, σ≥0 a stochastic field (called the energy dissipation field in turbulence and volatility in finance) and L a Lévy basis. Now, the ambit field Y is

Yt(x)=μ+∫At(x)g(η,s,x,t)σs(η)L(dη,ds)+∫Bt(x)q(η,s,x,t)as(η)dηds

Ambit sets

In the above, the ambit sets At(x) and Bt(x) describe the sphere of influence for a given point in space-time. I.e. at a given point, (t,x)∈χ×ℝ the sets At(x) and Bt(x) are the points in space-time which affect the value of the ambit field at (t,x),Yt(x). When time is considered as one of the dimensions, the sets are often taken to only include time-coordinates which are at or prior to the current time, t, so as to preserve causality of the field (i.e. a given point in space-time can only be affected by events that happened prior to time t and can thus not be affected by the future).

The ambit sets can be of a variety of forms and when using ambit fields for modelling purposes, the choice of ambit sets should be made in a way that captures the desired properties (e.g. stylized facts) of the system considered in the best possible way. In this sense, the sets can be used to make a particular model fit the data as closely as possible and thus provides a very flexible – yet general – way of specifying the model.

Ambit process

Often, the object of interest is not the ambit field itself, but instead a process taking a particular path through the field. Such a process is called an ambit process. As an example such a process can represent the price of a particular financial object – e.g. the price of a forward contract for a certain time and point in space, space representing things such as time to delivery, spot price, period of delivery etc.[2] This motivates the following definition:

Let the ambit field, Y, be given as above and consider a curve in space-time τ(θ)=(x(θ),t(θ))∈χ×ℝ. An ambit process is defined as the value of the field along the curve, i.e.

Xθ=Yt(θ)(x(θ))

Stochastic intermittency/volatility

The energy dissipation field/volatility, σ, is, in general, stochastic (called intermittency in the context of turbulence), and can be modelled as a stochastic variable or field. Particularly, it may itself be modelled by another ambit field, i.e.

σt2(x)=∫Ct(x)h(η,s,x,t)L~(dη,ds)

where L~ is a non-negative Lévy basis.

Integration with respect to a Lévy basis

The stochastic integral, ∫At(x)g(η,s,x,t)σs(η)L(dη,ds), in the definition of the ambit process is an integral of a stochastic field (the integrand) over Lévy basis (the integrator), and is thus more complicated than the usual stochastic Itô-integral. A new theory of integration was provided by Walsh (1987)[3] where integration is done with respect to random fields and this theory can be extended to integration with respect to so-called Lévy bases,[4] which is the main building block of the ambit field.

Definition of Lévy basis

A family (Λ(A):A∈𝔹b(S)) of random vectors in ℝd is called a Lévy basis on S if:

1. The law of Λ(A) is infinitely divisible for all A∈𝔹b(S).
2. If A1,A2,…,An∈𝔹b(S) are disjoint, then Λ(A1),Λ(A2),…,Λ(An) are independent.
3. If A1,A2,…∈𝔹b(S) are disjoint with ⋃i=1∞Ai∈𝔹b(S), then
Λ(⋃i=1∞Ai)=∑i=1∞Λ(Ai), a.s.

where the convergence on the right hand side of 3. is a.s.

Note that properties 2. and 3. define an independently scattered random measure.

A stationary example

In some data (e.g. commodity prices) there is often found a stationary component, which a good model should be able to capture. The ambit field can be made stationary in a straightforward way. Consider the ambit field Y, defined as

Yt=μ+∫At(x)g(η,t−s,x)σs(η)L(dη,ds)+∫Bt(x)q(η,t−s,x)as(η)dηds

where the ambit sets, At(x),Bt(x) are of the form At(x)=A+(x,t) where the time-coordinates of A are negative (same for B). Furthermore, we take g(η,t,x)=q(η,t,x)=0 for t≤0 and that σ and a are also stationary random variables/fields. In particular, we can take σ to be a stationary ambit field itself:

σt2(x)=∫Ct(x)h(η,t−s,x)L~(dη,ds)

where L~ is a non-negative Lévy basis and h is a positive function.

References

  1. ↑ 1.0 1.1 Barndorff-Nielsen, O. E., Schmiegel, J. "Ambit processes; with applications to turbulence and tumour growth", Research report, Thiele Centre, December 2005
  2. ↑ 2.0 2.1 2.2 Barndorff-Nielsen, O. E., Benth, F. E., and Veraart, A., "Modelling electricity forward markets by ambit fields", CREATES research center, 2010
  3. ↑ Walsh, J., "An introduction to stochastic partial differential equations", Lecture Notes in Mathematics, 1986
  4. ↑ Barndorff–Nielsen, O. E., Benth, F. E., and Veraart, A., "Ambit processes and stochastic partial differential equations", CREATES research center, 2010