Probab. Th. Re1. Fields 82, 137-154 (1989) Theory Probabilitywong/wong_pubs/wong100.pdfProbab. Th....

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Probab. Th. Re1.Fields 82, 137-154 (1989) Probability Theory Related Fields Springer-Verlag 1989 Isotropic Gauss-Markov Currents* Eugene Wong and Moshe Zakai** University of California, Collegeof Engineering,Dept. of ElectricalEngineering and Computer Sciences,Berkeley CA 94720, USA and Technion,Haifa, Israel Summary. A natural definition of the Markov property for multi-parameter random processes (random fields) is the following. Let {Xt, tEIR N} be a multi- parameter process. For any set D in N.N, let a D denote the a-field generated by {Xt, tED}. The field {Xt, tEN. u} is said to be Markov (or Markov of degree 1 [6], or sharp Markov) if, for any bounded open set D with smooth boundary, o- D and ape are conditionally independent given aOD. It has been known for some time that to find interesting examples of Markov processes under this definition; it is necessary to consider generalized random functions. In this paper we show that a natural framework for the Markov property of multiparameter processes is a class of generalized random differential forms (i.e., random currents). Our principal objective is to relate the Marko- vian nature of an isotropic gaussian current to its spectral properties. 1. Introduction The notion of a random r-current in IRN, 0_< r_ N, was introduced by K. Ito in 1955 [5] following the deRham notion of non-random currents (cf. [9]); it was motivated by the theory of statistical turbulence. The notion of a differen- tial r-form is a generalization of scalar (r= 0) and vector (r= 1) fields in N N (cf. e.g. [4, 12]), and the notion of currents generalizes differential forms by considering r-forms with coefficients that are generalized functions. In particular, a random 1-current is just a random vector field with components that are generalized random fields. A random current is said to be homogeneous (isotro- pic) if its second-order properties are invariant under translations (rotations and reflections). In [5], Ito presented a complete characterization of the spectral measures associated with homogeneous isotropic currents in terms of two posi- tive measures on (0, oo) and one constant, regardless of the space dimension * Work supported by the Army Research Office, Grant No. DAAG29-85-K-0233 ** Work done while at the Universityof California at Berkeley

Transcript of Probab. Th. Re1. Fields 82, 137-154 (1989) Theory Probabilitywong/wong_pubs/wong100.pdfProbab. Th....

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Probab. Th. Re1. Fields 82, 137-154 (1989) Probability Theory Related Fields

�9 Springer-Verlag 1989

Isotropic Gauss-Markov Currents*

Eugene Wong and Moshe Zakai** University of California, College of Engineering, Dept. of Electrical Engineering and Computer Sciences, Berkeley CA 94720, USA and Technion, Haifa, Israel

Summary. A natural definition of the Markov property for multi-parameter random processes (random fields) is the following. Let {Xt, tEIR N} be a multi- parameter process. For any set D in N. N, let a D denote the a-field generated by {Xt, tED}. The field {Xt, tEN. u} is said to be Markov (or Markov of degree 1 [6], or sharp Markov) if, for any bounded open set D with smooth boundary, o- D and ape are conditionally independent given aOD. It has been known for some time that to find interesting examples of Markov processes under this definition; it is necessary to consider generalized random functions. In this paper we show that a natural framework for the Markov property of multiparameter processes is a class of generalized random differential forms (i.e., random currents). Our principal objective is to relate the Marko- vian nature of an isotropic gaussian current to its spectral properties.

1. Introduction

The notion of a random r-current in IR N, 0_< r _ N, was introduced by K. Ito in 1955 [5] following the deRham notion of non-random currents (cf. [9]); it was motivated by the theory of statistical turbulence. The notion of a differen- tial r-form is a generalization of scalar ( r= 0) and vector ( r= 1) fields in N N (cf. e.g. [4, 12]), and the notion of currents generalizes differential forms by considering r-forms with coefficients that are generalized functions. In particular, a random 1-current is just a random vector field with components that are generalized random fields. A random current is said to be homogeneous (isotro- pic) if its second-order properties are invariant under translations (rotations and reflections). In [5], Ito presented a complete characterization of the spectral measures associated with homogeneous isotropic currents in terms of two posi- tive measures on (0, oo) and one constant, regardless of the space dimension

* Work supported by the Army Research Office, Grant No. DAAG29-85-K-0233 ** Work done while at the University of California at Berkeley

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138 E. Wong and M. Zakai

N and order of the form r (cf. [16] for an exposition of Ito's results and some further results).

A natural definition of the Markov property for multi-parameter random processes (random fields) is the following. Let {Xt, tER N} be a multi-parameter process. For any set D in RN, let a D denote the a-field generated by {Xt, t~D}. The field {Xt, t~IR N} is said to be Markov (or Markov of degree 1 [7], or sharp Markov) if, for any bounded open set D with smooth boundary, a D and ado are conditionally independent, given a0D. As was already noted by P. L6vy, this definition leads to a restrictive class of processes and excludes some interest- ing processes that have a weaker Markov property. One example of such pro- cesses is the L6vy Brownian motion in IR N with N odd, which, as conjectured by L6vy and proved by McKean [7], has a Markov property involving ( N - 1)/2 normal derivatives of the random field, that are generalized random processes. As was shown by Wong [13], it is possible and useful to define the Markov property for generalized (distribution valued) random fields. A general definition of the Markov property, namely the germ-field Markov property, was proposed in [7]. The idea is to define the germ a-field associated with the boundary aD by ,~OD = U a(3D~) where 0D, is the ~-neighborhood of OD and to define

~ > 0

Xt to be germ-field Markov if aD and ado are conditionally independent given ,roD. This definition has the advantage of being easily extendible to the case where X is a generalized field, while including many processes that are not considered Markov in the classical sense. For example, for N = 1, any collection of polynomials is germ-field Markov and so is the k th integral of the Wiener process. However, neither process is Markov in the classical sense. The theory of one parameter Markov processes deals almost exclusively with processes that are Markov in the classical sense and has very few results for processes that are germ-field Markov. On the other hand, the theory of multi-parameter fields deals mainly with processes that are germ-field Markov (usually denoted just Markov; cf. [6, 11]).

The purpose of this paper is to consider the Markov property in the frame- work of random r-currents. This approach reflects, in a natural way, the geomet- ric aspects of the problem and is supported by a powerful coordinate-free calcu- lus for these objects [9]. In the particular case of zero currents, namely general- ized scalar valued processes, the results of this paper also follow from known results for Markov fields (cf. e.g. [3] or Theorem 2 on p. 145 of [11]). The boundary a-field associated with certain random currents is defined in this paper, in a direct "geometric" way, avoiding the germ-field notion. The Markov proper- ty relative to this boundary field is defined and conditions under which a Gaus- sian isotropic random current has this Markov property are derived. In order to be able to define such a Markov property (in contrast with the germ-field Markov property), we consider a restricted class of random currents. Roughly speaking, the random currents that we consider have the property that when integrated on bounded subsets of (N-- 1) dimensional manifolds, they yield ran- dom variables. This gives a natural definition for the splitting sigma field asso- ciated with the boundary data. Currents for which integration on bounded subsets of (N-1) manifolds yields random variables will be called localizable

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Isotropic Gauss-Markov Currents 139

currents. This approach leads to a natural definition of the Markov property for such currents that seems to reflect well the geometrical nature of the problem. Scalar valued Markov (not necessarily Gaussian) processes on the plane were considered in [14], and it turns out that a natural parametrization for Markov processes on the plane is parametrization by paths rather then by points. This corresponds to localizable one forms in the plane and motivated the approach of this paper. Martingale properties of certain classes of random currents were considered in [15].

In the one-parameter case, a Gaussian stationary process {Xt, - oo < t < oo} with spectral density 1/P(v2), where P is a polynomial of order p, is, in general, not Markov. However, Xt, together with its ( p - 1 ) derivatives, form a Markov p-dimensional vector. The notions of localizability and Markov property intro- duced in this paper enable us to obtain results for general Gaussian random currents that reduce to this result when specialized to the one-parameter case. In the one-parameter case, a Gaussian process with spectral density Q(v2)/p(v 2) (where the Q and P are polynomials and the order of Q is lower than that of P) is, in general, not germ-field Markov, but can be embedded in a finite- dimensional Markov process as one of its components. It seems that this result does not have a general extension to the multi-parameter case. A partial general- ization to the case is discussed in the last section.

In the next section we summarize the results of [5] (cf. also [16]) and present a useful spectral representation for homogeneous and isotropic random currents [16]. The notions of random cochains, localizable currents and Markov currents are introduced in Sect. 3. Conditions for localizability on the spectral density are also given in Sect. 3. Conditions under which an isotropic random current is Markov or can be embedded in a Markov current are derived in Sects. 4 and 5. Section 4 deals with random currents that are either solenoidal or irrota- tional, and Sect. 5 deals with general currents.

2. Random Currents

In this section we summarize the results of random currents that will be needed in later sections (cf. [5, 16] for details). Let el , e2, ..., eN denote an or thonormal basis in IR N. We use i to denote a multi-index i= ( i l . . . . , it), with li[=r, ]il to denote a rearrangement of i that puts the indices in increasing order and i* to denote the n - r multi-index complementary to i in increasing order. A differ- ential r-form has the representation

q~r(t) = ~ q~i(t) el, t d R N (2.1) lil

where el = %/x % . . . / x % and @i(t) are sufficiently smooth functions (to be clari- fied later). The Hodge star operator* operating on q5 r is the N - - r form

* ~(t)= ~ d~i(t) ei*'c~ ( 1' 2' " " ' 9 I|1 i, i*

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140 E. Wong and M. Zakai

where 6 is I if (i, i*) is an even permutation of 1, 2 . . . . . N and - 1 if the permuta-

tionisodd. T h e e x t e r i o r d e r i v a t i v e i s d ( o , = ~ ( ~ e j / x e O . Theinteriorprod- uct e i v ej is defined by Ill J

e iv ej = *(el ^ *e j ) . ( - 1) (q-p)(N- q) (2.2)

[i[=p, I j l=q. Note that if lil=lJl then e ive i is scalar valued; in this case we shall also write (ei, ej) for (e~ v ej) and (ei, ej) can take the values 0, + 1 , - 1 only.

Whenever convenient, we use a coordinate system to represent the forms, currents, and operations under consideration even though in nearly every case, these quantities are intrinsic and the results obtained are independent of the coordinate system used to derive them [4, 12].

Let S denote the Schwartz space of fast decreasing functions on N~ N and S ~ the space of differential r-fo~ns as given by (2.1) with q~eS. A (non-random) r-current [9] is a continuous linear functional on S N-~ or, roughly speaking, an r-current is an r-form (2.1) in which the functions qS~(t) are Schv~artz distribu- tions.

A random current [-5] is a continuous linear functional from the (non-random) space S N-~ to the space of L 2 (possibly complex) random variables and a Gaus- sian random current is a random current for which these linear functionals are (possibly complex) Gaussian random variables. Let M be a random zero current, i.e., a random Schwartz distribution. M is said to be a random measure if for every pair ~b, OeS.

EM(O) MC(~O) = ~ q~(t) ~U(t) m(dt) (2.3) Rlv

for some slowly increasing measure m(dt) on IR N where ( )c denotes the complex conjugate when applied to numbers and the complement when applied to sets. A random measure M can be extended to be a functional on indicator functions of Borel sets E in R N with EM(E'). M(E')= m(E'n E"). Therefore, in the Gaus- sian case the random set function M is of independent increments and M(qS) = ~ gp(t) M(dt). A random r-current M~ is called a random measure of degree

RN

r if there exist slowly increasing measures on ]R N, m~,j(dt), li[ = ] j l = r , such that for 4,, OeS.

E {M~(~b ̂ (*ei))-M~(~/x (*ei)) = ~ qS(t) Or mi, j(dt)}. (2.4)

Let h denote a point in IR N and consider the shift (Zh q~) (t) = q~ (t + h). A ran- dom r current U~ is said to be homogeneous if for all h,

E ( ~ (0N - , ) Ui (~N - 3) = E (U, (zh ~ , , - ,)" ~c (rh ~ , , - ,)).

Let pi, i(~b, ~k~S) denote

Pi, j (~b ~//) =E(Ur(O" ei,) U~C(~ '- ej,))

(2.5)

(2.6)

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Isotropic Gauss-Markov Currents 141

p is called the covariance bilinear form (or the covariance double current) asso- ciated with U. The main result regarding homogeneous random currents is as follows. Let q~ denote the Fourier transform of ~b, q~(v)= ~ exp- i (v , t) ~b(t) dt.

RN

The covariance bilinear form of any homogeneous r-current can be written a s

p,j(q~, ~k)= ~ q~(v).~:(v) mij(dv). (2.7) RN

Furthermore, there exists a random r-measure Mr such that

U~(~b ̂ el,)= Mr(~9 A ei,), (2.8)

Mr and m,.j are called the random measure and spectral measure associated with U~ respectively.

Every smooth non-random vector field ( r= 1) in a domain in IR N, N = 3 , can be represented as the sum of a constant (position independent) vector field, a gradient of a scalar potential (zero form) and the curl of a vector potential. The generalization of this representation for homogeneous random currents with general r and N will now be considered. Let the exterior derivative d and the Hodge star operator* on U be defined as follows:

(d U~) (q~) = ( - 1)r + ' U~(d q~), ~ s S N-r-1 :

(*Ur) ( ~ ) = ( - 1)r(N-r)(Ur(*~))r ~S ~

6 U~ = ( - 1) Nr +* +1 (*d* Ur). (2.9)

The spectral measure Mr associated with the homogeneous current U via (2.8) / k4 - - M ( ~ 4- M O ) .4- M(s) can be decomposed into the sum of 3 spectral measures -,-r----~ - - , - r --.-~

where

M~~ = Mr(A n {0}).

Let M~ "~ denote the difference -.- ra/t(u) _- -.- - ---rM(~ and for v + 0 set

(2.1o)

M~ 0 (d v) = v A (v v M~ u~(d v)) iv12 = e~ ̂ (e~ v M~U)(dv)), (2.11)

M(~ s) (d v) = v v (v ̂ M(~ u) (d v)) iv12 =e~v(e~AM~")(dv)) (2.12)

V where e~ = ~ is the unit vector in the direction of the vector v (which is the

vector connecting the point 0 to the point v in ~,N). Then [5, 16]

Mr(dr) = M~~ + M~~ + M~)(dv).

Let U (~ U (~ U (s) denote the homogeneous random currents corresponding to the spectral measures M (~ M ~i), M ~) respectively. Then U = U ~~ + U(~ U (s),

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142 E. Wong and M. Zakai

U ~ is called the invar ian t par t of U(U~ �9 e i ) = U(~ ei) for all fixed -c in IRN), U (~ is called the irrotational par t of U, and U (~) is called the solenoidal par t of U.

Let e~ . . . . , en be an o r t h o n o r m a l basis at the po in t v in N N such tha t el =e~, where e~ denotes the unit vector in the direct ion f rom the origin to v. Then, every r - form 4)=ZqS~.e~ can be d e c o m p o s e d into two componen t s , one c o m p o - nent s is the sum over all mult i- indices i = [i] such tha t i~ = 1 and the other c o m p o n e n t is the sum over all i = [i] such tha t i~ + 1. Then M~~ as defined by (2.11) is the sum of all c o m p o n e n t s of M~ ") in which i 1 = 1 and M~)(dv) is the sum over all mult i- indices i which do not include i 1 = 1. This decompos i t ion of a cur rent into a) the sum of componen t s , including (locally at po in t v) e~ in % and b) the sum of c o m p o n e n t s which locally at v do not include e, in e, plays a key role in the represen ta t ion of i sot ropic currents which we consider next.

Let G denote the full g roup of o r t hogona l t r ans fo rmat ions ( rotat ions and reflections) in N N. F o r g~G, let a , U~ denote the t r ans fo rma t ion on U~ induced by g, i.e.

and ag[~N-~] is the t r ans fo rma t ion on the differential fo rm q~N-r induced by g (ag(~bi(t)-ei, A ... A ei) = qSi(g" t). g - 1 ei ' A ... A g - 1 ei). A r a n d o m current /.Jr is said to be i sot ropic if, for all g e G , q~, ~ 6 S N-~

E(~(q~) ~c(0)) = E~. ur(4,) (~ u~. (0)) ~. (2.~3)

Consider the spectral measure mi, i(d v), l i I= I j l = r associa ted with a h o m o g e - neous and i so t ropic current , and assume for the r emainder of the paper , tha t M ( ~ 0. Assume tha t at po in t v in N~ N the coord ina te sys tem is such that e, = e l , then it follows f rom i so t ropy tha t ml, j(dv)=O for [i] :t: [ j] . I t also follows f rom i so t ropy tha t there are at mos t two different values for m~.i: one for l c i and ano the r for 1 r This yields the following:

The Ito representation ([-5], cf. [16].) Let e l , e2, . . . , eN be any o r t h o n o r m a l coor- d inate system. Then the spectral measu re of any h o m o g e n e o u s and isotropic current is expressible as:

mi, i(d v) = (e~ v % e~ v ei) m (0 (d v )+ (e~ A el, e~/~ ei) m (s)(d v). (2.14)

(Recall tha t for l il = l] I, (ej, e j )= (el v ei)), where m (i) (d v) and rn (s) (dr) are two spher- ically invar ian t measures on IR ~. Tha t is, if g is any ro ta t ion or reflection in NN, then m(~ m(~)(A) and m(~)(gA)= rn(~)(A) for every Borel set in IR N. F o r every spherical invar ian t measu re m(dv) we can write

m (d v) = 2 N- *. t/(d 0) F (d 2) (2.15)

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I s o t r o p i c G a u s s - M a r k o v C u r r e n t s 143

where 2 = Ivl, 0 =-v is a point on the unit sphere in IR N and rl(dO) is the uniform 2

measure on S N-1 (the unit sphere in IR N) with total measure ~/(S N-l) N -1

= 2. zdv/2 (F (~-)) .Hence

m ") (d v) = 2 N- 1/1 (d O) f o (d 2), (2.16)

m (s) (d v) = 2 N- 1 q (d 0) F (s) (d 2) (2.17)

and ml, j(dv) is determined by the two measures on (0, oo), F (~ and F (s) on (0, oo). If r = 0, then m (i)- 0 and if r = N then m (*) - 0.

A Sample Function Representation for U~ [16]. If U is a homogeneous and isotropic r-current, then there exist a r andom ( r - 1) measure Y(dv) and a r andom ( N - r - l ) measure 2(dr) such that ~ and 2 are uncorrelated and for every ~)N_reS N-r and i, with lil = r

iv iv ^ U~(~bu_r)= ~ q~N_~/x~-,x Y(dv)+ ~RN*~)N_~A~AZ(dv) (2.18)

N N I

where q~ denotes the Fourier t ransform of 4): if ~b = Z qSi. ei then q~ = Z q~i e~ where q~ is the Fourier t ransform of function q~i(t)). ~'(d v) = ~ ~ (d v), ]i[ = r - 1 and

[q

E~(dv)(~(dv')) c=fO' if [ i ] ~ [ j ] (2.19) [m"~(dv~dv), i = j

where m")(dv) is as in (2.16). For ]i] = N - r - 1,

EZ~(dv)A (Zj(dvA ,))c q(0, if [i] 4: [j] (2.20) =lm(~)(dv c~ dr'), i = j

and m(S)(dv) is as in (2.17). The first term in the right hand side of (2.18) is the irrotat ional component of U and the second term is the solenoidal compo- nent. ~'= 0 if r = 0 and Z = 0 if r = N. For intermediate values of r, Y, 2 are defined as follows:

~'(dv) = e~ v M~(dv) a + e~/x W~(dv) Z(dv) = *(e~ A M~(dv)) + *(e, v Wb(dv)) (2.21)

where M~ is the r andom measure associated with U~, W"(dv) is a r andom ( r - 2 ) measure independent of M~ and satisfying

~ , qfO' [i34 =U] (2.22) EW~"(dv) i=j, ] i]=(r--2)

and W b (d v) is a random (r + 2) measure independent of M~ and IV", satisfying

b , (0, [ i ]4:[J] (2.23) EWib(dv) rWj (dr)=~m(~)(dvc~dv'),l i=j, l i l= ( r+2) .

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144 E. Wong and M. Zakai

3. Random Cochains, Localization and the Markov Property for Currents

Let D be a bounded open set with smooth (C | boundary OD; the a-field generat- ed by a random r-current U~ on D is defined to be the a-field generated by { Ur(qS), supp. q~ = D} and similarly (with D replaced by O c) for the o--field generat- ed by U~ on D c. In order to consider the Markov property of random r-currents relative to D, OD, D c we have to define what is meant by the boundary data. The notion of the boundary data will now be defined for a class of currents for which this data has a concrete meaning (cf. also [-14] and [-15]) and conditions will be derived under which homogeneous currents belong to this class.

Let V be an r-dimensional C ~ manifold in ]R N and let c be a chain in V, (i.e., c is a finite linear combination of simplexes on V) then ([9] Sects. 9, 10) c defines a (non-random) N - r current in the sense of deRham and there exists a sequence of ( N - r ) differential forms ~k, k = 1, 2 . . . . . t, kk~S N-r such that ~k k ~ c in the sense that

I ~kk^ ~b ~ I ~ b (3.1) p. /v c

for every q~eS r and the convergence is uniform for any collection of forms ~b that are bounded on S r. A collection of forms ~b on S r is said to be bounded if the support of all the ~b's is contained in the same compact set K where K itself is contained in the domain of some coordinate system and all the partial derivatives of every coefficient of each ~b are bounded in absolute value on K.

Definition. A random r-current U, is said to be a random r-cochain if, whenever c is a bounded r-chain and ok ~C, okesN-r then the sequence of random vari- ables U~(O k) is a Cauchy sequence in L 2.

If X is an r-cochain, r = N - 1 , and 0D is a C ~~ compact manifold, then X(c) is a well-defined random variable for a rich class of r-dimensional subsets c of 0D and this will be used later to define the a-field of the boundary data on 0 D. For the case where r < N - 2 , the fact that X is an r-cochain will enable us, as will be shown later, to define the sigma-field of the boundary data on OD. We shall also consider cases where U~ is not extendible to an r-cochain, but can be extended to become an (N--l)-cochain, which will then suffice to construct the a-field of the boundary data. For example, consider an / -cur ren t in N = 3 dimensional space such that integration along lines does not yield random variables, but integration first along lines and then along a perpendicular path yields concrete random variables parametrized by N - 1 dimensional sub- sets of OD. These r.v. can then be used to define the sub-a-field of the boundary data.

Let U, be an r-current and let an_,_ 1 be a fixed N - r - 1 covector, then for any fixed 1-vector bl and any c~S, c~.blAaN_r_l is in S N-r, hence (aN-r+ 1 ̂ U,) (q~ ̂ bl) = Ur(q~ ̂ bl ^ aN-,+ 1) and (aN-r+ 1 ̂ Ur) is a well-defined (N-- 1)-current.

Definition. An r-current U~, 1 <_r<_N--1, is said to be localizable if for every fixed (N-r-1)-covector aN-,-1, the (N--1)-current aN-,-1 ^ Ur is a cochain

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Isotropic Gauss-Markov Currents 145

and for every ( r - 1 ) covector at-1 the (N-1 ) - cu r r en t a~_ 1/x (*U,) is a cochain. A zero current U is localizable if aN-1 A U is a cochain and an N-current is localizable if *U is localizable. Note that for 1 - < r - < N - 1 , every r-cochain is localizable.

Let U be a localizable random r-current and V a C*(N - 1)-manifold in IR N. Let V~ denote the collection of bounded ( N - 1) chains in V.

Definition. The boundary data of U on V is the sub-a-field generated by

~aN_r_l/xU and ~ar_aA(*U) C C

for all ce V~ and all fixed covectors aN-,-1 and a,_ 1, i.e.,

av(U)= a{ ~ aN- , - 1/x U, ~ a~-I A (*U), c6 V~}. c c

(3.2)

Remark. It is indeed natural to define aoD(U ) via U(c), ceV~. The reasons for including (*U)(c) in the definition are as follows: (a) Let qS=~b i ( t ) e i be an

lil r-form with q~i(t) random and well-behaved (say c ~~ then the a-field generated by ~b on a D will be

o-{~bi(t), t~OD, li[--r}

and the extension of this to currents calls for the inclusion of *U. (b) For scalar valued Markovian fields X, i.e., zero currents, an important role is played by (cf. e.g. [-7, 8], Chapt. 3 of [-11, 3J). More specifically, the minimal splitting a-field generated by the integral of 8X/Sn (and higher derivatives) on subsets of the boundary which is an N - 1 dimensional manifold is the same as the integral of *dX on this subset. Consequently for the particular case of zero currents, the results of this paper also follow from the previously known results cited above. It is when the Markov property of higher order currents is consid- ered that the advantage of the calculus of currents becomes clear.

We define now, the Markov property for localizable currents, as follows:

Definition. Let U=(U~(~ ), U~ ), ..., U~ )) be a collection of localizable currents of order rl . . . . . rp respectively (which may be equal or not). U is said to be Markov if for every connected and bounded domain D with smooth boundary 0D, the a-fields generated by U on D and D c are independent given the boundary a-field generated by { U~, i = 1, 2 . . . . , p}.

Remark. This definition generalizes the notion of "Markov of order p" given in [7] (cf. also [-8, 14]).

We conclude this section with some conditions under which homogeneous currents are cochains or localizable. Consider the case where U is an homoge- neous current. Assume that the spectral measure mi, i(dv ) associated with U is absolutely continuous with respect to the Lebesgue measure on ]R N.

ml, j (dr ) = #i, j (v) d v (3.3)

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146 E. Wong and M. Zakai

Proposition 3.1. Let

K Iml,j(v)l < (3.4)

= ivl2moP(ivl2)

for all i,j with IJl=lil=r where P(.) is a polynomial of degree p>=O with non- negative coefficients and P(O) =~ O.

(a) I f mo= 0 and ( N - r ) < p then U is an r-cochain. (b) l f N - - r<p+mo and N > 2 m o then U is an r-cochain. (c) I f N> 2mo and p+mo > 1 then U is localizable.

Proof Let c be a chain as discussed earlier, since c defines an ( N - r ) current it possesses a Four ie r t ransform, say C(v)=~Ci(v)el. Assuming that P ( 0 ) > 0 , then (3.4) implies that i

I~i, j(v)l _-< K1 (1 + Iv12) -p

for some K 1. In order to show that U(O k) converges in L 2, it suffices t o show that for all i, Ill = N - r ,

IG(012 K1 R~, (l+[v[2) p d v < ~ (3.5)

(since e-I*lZ/kC(v), k ~ , can serve as ~k). Fo r p > N - r , (3.5) follows f rom par t b of Theo rem IX.39 of [10], which proves par t a. Regarding par t b, we have to show that for all i, Ill = N - r ,

K1 IC'(v)12 (1 + Iv12) p+"o d r < ~ (3.6)

RN

and

f. I v l -Zm~ ~ . (3.7) Ivl<l

Now, (3.6) follows by the same argument as (3.5). As for (3.7), by (2.15)

1 Ivl- 2m~ N'~U/2(F(N + �89 - ~ ~ s 2m~163 ~ d2

Ivl__<l o

and (3.7) is satisfied for N - 1 - 2 m o > 0 . Finally, (c) follows from (a) and (b) by specializing to r = N - 1.

4. Isotropie Gauss Markov Currents I

We shall use (*d)mX to denote (*d)~ ( * d ) l X = * d X , (*d)ZX=*d(*dX) , etc. No te that if X is an r-current , then (*d)mX is an r-current for m even and an N - r - 1 current for m odd.

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Isotropic Gauss-Markov Currents 147

Theorem 4.1. Let X be a Gaussian homogeneous and isotropic r-current in N. N, r> l, with Fo-O,F(~)=O, and F(~176 where m o is an integer satisfying

-- 1 < mo _-< ( N - - 3)/2

and P is a polynomial of order p with P(0) =t= 0, i.e.

mi, j(dv) = ((e~ v ei), (e~ v el) ) �9 (Ivl2m~ dr2.., dVN.

Then there exists an ( r - 1) current Y such that X = d Yand

{(*d)" Y, m = 0, 1 . . . . , (p + too)} is Markov.

Remark. Theo rem 4.3 extends the result of this theorem to m o = [ ( N - 1)/2]�9

Proof. (a) No te that by Propos i t ion 3.1, (*d) m X, 0 < m < p + m o - 1, is localizable. Set

Y(c~)= ~ ~(v)/~ ,1, Y(dv) (4.1) R N I V l

where If is as defined in equat ions (2.17) and (2.18) and 0 ~ S N-~ + 1, then X = d Y and by Propos i t ion 3.1 Y is also localizable.

(b) Fo r further reference we note the following two well known lemmas:

L e m m a 4.1. Let W be the Fourier transform of a random measure M;

E{W(qS) W~(~9)}= ~ ~a(v)~C(v)m(dv) (4.2) R N

qS, t ~ S . Assume that m is spherically invariant (re(A)= m(gA)) and consequently re(d2) = tl(dO) p(d2). Then

E{W(40 We(C)} - ( N - 1 ) r c ~ lim i ~ dP(x)~C(Y)

/ - b __+ oo a

J~N-2)/2 (2~2 [x--yl) 2N_ 1 d x d y p ( d 2 ) (4.3) (2~,~lx- yl)(N- e)/2

where "In is the Bessel function of order n. Furthermore, for any multi-indices ~, fi

a x ~ = a x ~ , �9 a ( x o ~ ' 1~1 = z ~

E W q5 W ~ 1)1~1(--1) I ~ l ( N - 1 ) ~ * b

�9 lira ~ ~ q5 (x) ~ (y) 4, r (N+I ) ;5oo ~Nx~,,

2

~ J J~N-2)/2(2~'~Ix--yl) 2N_~p(d2)" (4.4) Ox ~ ~xP (2rc2]x--yl)(N-2)/2

The p roo f of this result is s t ra ightforward and therefore omitted�9

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148 E. Wong and M. Zakai

Lemma 4.2. I f the assumptions of the previous lemma p(d)O=d)~/P()c 2) where P is a polynomial of order q, then

E{W(P(--A)O)'WC(O)} = ~ ~ ( t ) ~ ( t ) dr= ~ ~)(t)Oc(t) dt NN N N

(4.5)

0 2

where A is the Laplacian operator Z i ~ . Furthermore, let D be a bounded domain

in ]R s, let O eS be f ixed and assume that the support of ~ is in the interior of D. Then there exists a function R(x, t~), x e D c such that

(i) R(. , r is C ~ on D ~. (ii) D(--A)R(t , t~)=O teD c.

(iii) For any ~ e S with support in D ~,

E(W(~)) WC(O))= ~ R(t, ~) ~)(t) dt R N

Proof of Lemma 4.2. Equation (4.5) follows from Eq. (4.2). Turning to R(. , ~) for a fixed x, we let R (t, ~) denote the generalized function satisfying

E{W(q~) WC(O)} = R((ib, ~)

in the distribution sense. Then, since the supports of q~ and ~k are disjoint, it follows by (4.6) that

E ( W ( P ( - A) c~) WC(~)) = 0

and over D c

P ( - A) R(. , q~)= 0

in the distribution sense. The existence and properties of R(. , q~) follow now from the fact that P(--A) is hypoelliptic (cf. e.g. [1], p. 66) and weak solutions are in fact C ~~ solutions.

(c) We now show the Markov property for r = 1, by reducing the problem to an interior Dirichlet problem and applying the results of part (b). Set P~ (x) = x I +,~o p (x). Since mo > - 1, P1 is also a polynomial.

Let D be a bounded domain in N~ N with smooth boundary 0D. Consider the problem of solving P1 ( - A ) f ( t ) = 0 , teD subject to the boundary conditions {(~"f (t)/~3 t") = h" (t), t e c~ D, m = 0 . . . . , m o + p} ([ 1] p. 91-93, [7]). It is more conve- nient for our purposes to rewrite the boundary conditions as follows: let h"(t), teOD, O<=m<=p+mo denote a zero form on aD for m even and an N - 1 differen- tial form on ~D for m odd. It is required that ((*d)mf(t))oD, i.e., the restriction of (*d)"f(t) to the boundary, satisfy

(*d)mf(t)=h~(t), teOD, O<m<p+mo. (4.6)

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Isotropic Gauss-Markov Currents 149

Note that (*d)2m=(A) m that *df is an ( N - 1 ) form, and the integral of *df on subsets of the surface t l = 0 , (t=t 1 .... , tN) yields the integral of the normal derivative o f f ( t ) on this surface.

For smooth boundary data the Green function solution to PI(-A)f=O subject to (4.8) is as follows [1]: given any t in the interior of D, there exist gt('), O<m<-<-p+mo that are smooth ( N - l ) differential forms on OD for m even and smooth zero forms for m odd, parametrized by t, such that

p4-m 0

f(t) = ~ ~ h"/x g~' (4.7) m=O 8D

solves P1 ( - A ) f = 0 in D and satisfies (4.6), c.f. [3] for an extension of the solution of PI(-A)f=O subject to boundary data which are generalized functions. In our case, we have the function R(t, ~), teD, the support of ~ is in D e, and for P~(- A) R(t, 0)=0 , teD. Equation (4.7) is, in this case

p + m o

R(t, t~)= ~' I (*d)mR( ", O) A g~'('). (4.8) m = 0 c~D

If Yt were a smooth random process, we could write

(*d)mY/xg~) YC(O =R(t,~)-- ~ ~ (*d)mR(O, tp)Ag~fl(O) (4.9) m = l OD m=O ~D

The right hand side of the last equation is zero by (4.8) and therefore, the Gaussian random variables Y(q~) and

p+mo

Y~-- ~, ~ (*d) m Y/x g~' (4.10) m = l aD

are independent. Consequently, Y(O) and Y~ are independent, given the boundary data {(*d)my, m = 0 . . . . ,P+mo on OD}. Hence {(*d)m Y,m-0 , . . . ,p+mo} is Mar- kov. In the general case, (still r = 1), Y, is a generalized random variable. Let q~eS and the support of ~b is in the interior of D. Then, by (4.8) and the smooth- ness of g

P+mo

E(Y((~) YC(~))=R((~,tp)= ~ ~ (*d)mR(',~)Ag~(.) (4.11) m = O ~ D

where go= S g(t)O(t)dr. Note that by (2.18) the stochastic integrals N N

(*d)~ 'Y( ' )^ g~( �9 ) 8 D

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150 E. Wong and M. Zakai

are well defined and satisfy

E y c ( ~ ) ~ (*d)mY(')Ag~(') = ~ (*d)"R( ' ,4)Ag~( ' ) . OD OD

Consequently, by (4 .11)

( / p+mo (4.12)

and therefore the Gaussian random variables Y(q~) and Y(O) are conditionally independent, given the boundary data, proving Theorem 4.1 for r = 1.

(d) Until now we have considered the case r = 1, for which Y is a zero form. For general r, Y as defined by (4.1) is an ( r - 1) current with independent compo- nents. That is, Y = X Y i . e i , f i l = r - 1 , where Yi is defined as follows: For qS=S~bl, where ~b is an g - ( r - l ) form, set Yi(~bl.)= Y(~bi.) and for [j]=~[i], Yi(~bj,)=0, then Yi and Yj are independent (I-i] Je [j]). Because of the independence of Yi, [i] = r - 1, it suffices to prove the theorem for some fixed multi-index io, ]io[= r - 1. Now, Y~o can be considered as a zero current and the results of the previous parts of the proof apply. The only question that remains to be settled is whether the sub-a-fields generated by {(*d)"Yio, O < m < p + m o } with Yio considered as an r-form and as a zero form are the same. Let Y~o ~ denote Yio considered as a zero current, namely for all ~b e S. Then we get

Y~~ (~b) = Y~o (~ �9 e,;). (4.13)

Therefore the sub-a-fields a { Y i ~ s u p p ~ ) ~ D } and a{Yio(q~.e,,), q~S, supp ~b cD} are the same. Turning to the boundary data, let Y be a 1-form and let Y~--YI. Then the integration of the one form I11 along a path in a hyperplane perpendicular to the tx-direction is zero while the integration of yo will yield a nonzero random variable. However, by (3.2) the N - 1 form "I11 can be integrated on a subset of the hyperplane perpendicular to ti . Conse- quently the boundary data of I11 and yo are the same on subsets of an ( N - 1 ) hyperplane. Similarly, by (3.2), the same arguments extend to subsets of an N - 1 manifold, and consequently the boundary data of Y1 coincide with that of yO. The same arguments apply to the case where Y is an r-form, r > 1, which completes the proof.

Theorem (4.1) dealt with irrotational currents. For solenoidal currents we have:

C o r o l l a r y 4.2. Let U be an isotropic and homogeneous r-current in IR N, r <= N - - 1 with Fo=0, F (~ and F(S)(d2)=(22m~ with mo an integer satisfying - 1 ~ mo _-< ( N - 3)/2 and P ( ' ) a polynomial o f order p with P(0) ~ 0, i.e.

mi, j = ((G A ei) , e v A ej) (Ivl2"~ P([v[2))- l dvl . . . . , dv N

Then there exists an ( r + l ) current Z such that U = * d * Z and {(d*)~Z, m = 0, 1 . . . . . (p + mo)} is Markov.

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Isotropic Gauss-Markov Currents 151

Proof. Note first that it follows from (2.14) or (2.17) that *U is also homogeneous and isotropic. Set *U = X, then X satisfies all the conditions of Theorem 4.1. Set Z = * Y where Y is as defined in Theorem4.1, hence {(*d)m*z, m = 0 , 1 , . . . , ( p + m o ) } is Markov. Now (*d)"*Z=*(d*)mz and {(d 'Z)", m = 0, ..., (p + mo) } is Markov since the sub-o--field generated by a localizable cur- rent, say W, on 8D (or D or D c) and the one generated by *Ware the same.

Theorem 4.3. Let X be as in Theorem 4.1 (Cot. 4.2) with mo = [ (N -1 ) /2 ] , then the results of Theorem 4.1 (Cot. 4.2) hold.

Remark. For the case r = l , p(22)= 1, and N odd, the one current X is the gradient of L6vy Brownian motion (cf. Eq. 7.2 of [5] or p. 129 of [11]), the zero form Y introduced in the proof is, in fact, the L6vy Brownian motion and Theorem 4.3 reduces to the result of McKean regarding the Markov proper- ty for Y for odd N.

Proof. By Proposition (3.1), (*d)X is localizable for 0 < m < ( p + m o - 1 ) as in the case of Theorem 4.1. Assume first, r = 1 ; in order to assure that Y is localiz- able, set

e i v t _ e i V t o

Y,= Ivl

where to is some fixed point in NN and ~(dv) is as defined in (2.19). Note that in this case we still have d Y = X . Furthermore, EI Y, I2< oo. Therefore Yt is a concrete random variable. Set EYt Y~C=R(t, s), then

(ei~t--e ivt~ (e-i~t--ei~t~ dv e(t, s)= S ivl2 ivl2.,oe(lvl2)

p .N

Operating on the t variable with the differential operator (-A)m~ yields, in the distribution sense,

((--A)~~ S ei~t(e-i~-e-i~t~ - 6 ( t - t o ) R N

Therefore, by the hypoellipticity of ( - A ) " ~ (p. 66 of [1]), it follows R(t,s) is C ~ outside the two points t=s and t=t o. For the case where D is a bounded domain on t and D does not include the point to, we continue as in the proof of Theorem 4.1. If toED then we have to consider the exterior Dirichlet problem rather than the interior one (as in [7]). The rest of the proof is the same as that of Theorem 4.1.

5. Isotropic Gauss Markov Currents II

In this section we consider the case where both components, F (i) and F (s) are present.

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152 E. Wong and M. Zakai

Theorem 5.1. Let X be a Gaussian homogeneous isotropic r-current with F(i)(d2) =FtS)(d2)=P(22)) d2, where P( . ) is a polynomial of order p. Let m o denote the

P

lowest power of the polynomial (P(x) = ~ ~q xq). Then for N - 1 => 2mo, m o

{(*d)JX, O<j<=p- 1}

is Markov.

Remark. The special case r = 0, p = 1 is known as the Free Euclidean Field.

Proof By Proposition 3.1, {(*d)JX, O < j < p - 1 } is localizable. Let e be any unit vector; then it can be verified that (e v el, e v ej) + (e/x el, e A e~) = (% ej). There- fore, since F(~ it follows from (2.4) that the components of X are independent, i.e., Xi(tb) is independent of Xj(t)) whenever [i] + [j]. Because of the independence of X~, ]i[=r, it suffices to prove the result for some fixed multi-index io. F rom here on, the proof is the same as the proof of Theorem 4.1 and therefore omitted.

Remark. While Theorems 4.1 and 4.3 are similar in the sense that to the given r-form X we adjoin an ( r - 1 ) form plus other forms which are ( N - r - 1 ) and r-forms, in Theorem 5.1, no ( r - 1) form is needed. The proofs of the three theo- rems are similar and is based on concentrating on the process with independent components which generate the r-current.

A partial converse to Theorem 5.1 is the following:

Proposition 5.2. Let X be a Gaussian homogeneous and isotropic 1-current with

F (0 (d 2) = c 1 2 u - 1 (~2 -t-/~2)- 1 d 2

F (~) (d2)= Cz 2 u - 1 (c~2 + 22) d 2.

(5.1) (5.2)

Assume that c 1 + 0, c 2 ~e 0 then X is Markov if and only if c 1 = c2.

Proof By Theorem 5.1 for c1=c2, X is Markov. Conversely, it is well known (cf. [113 :, p. 179) that an homogeneous vector valued generalized random field {X(t), t~iR N, X~IR d} with spectral density matrix f (v) satisfying ]lf-l(v)ll (lq-]V]2)-k~L1 for some k is germ-field Markov if and only if for any x, y ~ R d x r f - l ( v ) y is a polynomial in v. We show now that X is not germ-field Markov. Let I denote the unit N • N matrix and B(v) the N x N matrix with entries

(B(v)i,j-- vi vii v lL

By Ito's representation (2.14) and (5.1), (5.2) m(dv)= C(v)dv where

C (v) = (c21 + (cx - c2) B (v)). (ct 2 + I vl 2)- 1.

We show now that C-1 (v) is given by D (v) where:

(5.3)

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Isotropic Gauss-Markov Currents

The proof is as follows, by direct multiplication:

=/§ i+- cl) Now

B 2 (V) = B (v) since

(C2 - - Cl)2 B2 (v).

c l c2

153

(5.4)

(vlt (vxt B2(v) = i (vl, vN) ! (vl, v N ) ' -

\ V N / \ V N /

1(.) ivl 2 i ( v , , . . .

\ V N /

, vN) = B ( v ) .

Substituting into (5.4) yields D. C = 1. The (i, i) th entry of D (v) is

2 / 1 / 1 1 \ v z \

which is a polynomial in v only if c1=c2. Hence for C1:~=C2, C l : ~ 0 , Cz=~0 , X is not germ-field Markov and consequently not Markov in the definition of the present paper. Note that for c~ = 0 or c2=0, c(v) is singular and the result quoted from p. 179 of [-11] is not applicable.

Proposition 5.3. Let U be a Gaussian homogeneous and isotropic r-current with F~i)(d2)=F(S~(d2)=Q(24)/p(22) where P is a polynomial or order p and Q is a polynomial of order q < (p-1)/2. Then U can be embedded in a Gauss-Markov, homogeneous and isotropic r-current, i.e., there exists an isotropic and homogeneous Gauss Markov r-current X such that U is a linear combination of {(*d)JX, (d*)j X, O<=j<p- 1}.

Proof Note that if A is an r-form, then (*d)kA is an r-form for even values of k and an ( N - r - - 1 ) form for odd values of k and consequently we can take linear combinations of (*d)k'(U, (*d)k2U~ etc. if all kj are odd or all kj are even.

Let X be as defined by Theorem 5.1 with the same P as in the present proposition. Then by Theorem 5.1,

(*d)JX, O<=j<p-1

is Markov. Applying Theorem 5.1 to *X yields that (*d)J*X, O < j < p - 1 and consequently (d*)~X, 0 < j __<p- 1 are also Markov. We claim that

{(*d)JX, (d*)JX,j=O, 1 . . . . . p-- 1} (5.5)

is also Markov. To see this, note first that the ~r-fields generated by (*D)JX and *(*d)JX=(*d)J*X,j=O, 1 . . . . . p - 1 on D (and on D c) are the same. Now the ~r-field generated by (d*)JX on OD is in D (and D 0 by continuity, hence (cf. Lemma 1.3 a of [6]) (5.5) is Markov. Let A be the generalized Laplacian

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154 E. Wong and M. Zakai

A =df+6d, then A = _+((*d)2+(d*) 2) where the + or - signs are determined by N and r. Therefore, since 6 2---= d 2 = 0,

AS= _ ((*d)aJ-I- (d*)2J).

Note that if X is an r-current, so is AJX and since X(q~)=M(q~) then ([5] or gq. 4.13 of [16]), (AJX)(q~)= +M(lvl2Jq~). Let Q(lv14)=l(21(lv12)[ 2, set /~(~b) =M(Q 1 (Iv[ E) q~"), then U is a linear combination of ASX, hence a linear combina- tion of ((*d)JX, (d*)~X, 0 < j < p - 1 ) . Now U as defined in the statement of the present proposition has the same second-order properties, as U and since U and U are both Gaussian and they have the same probability law. Therefore U can be written as a linear combination of components of a Markov process, which completes the proof.

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Received February 15, 1987