• <tr id="yyy80"></tr>
  • <sup id="yyy80"></sup>
  • <tfoot id="yyy80"><noscript id="yyy80"></noscript></tfoot>
  • 99热精品在线国产_美女午夜性视频免费_国产精品国产高清国产av_av欧美777_自拍偷自拍亚洲精品老妇_亚洲熟女精品中文字幕_www日本黄色视频网_国产精品野战在线观看 ?

    Time Discrete Approximation of Weak Solutions to Stochastic Equations of Geophysical Fluid Dynamics and Applications?

    2017-07-02 07:17:18NathanGLATTHOLTZRogerTEMAMChuntianWANG

    Nathan GLATT-HOLTZ Roger TEMAM Chuntian WANG

    (Dedicated to Haim Brézis on the occasion of his 70th birthday)

    1 Introduction

    The primitive equations(PEs for short)of the oceans and the atmosphere are a fundamental model for the large scale fluid flows forming the analytical core of the most advanced general circulation models(GCMs for short)in use today.In recent years,these systems have been a subject of considerable interest in the mathematical community not only because of their wide significancein geophysical applications but also for their delicatenonlinear,nonlocal,anisotropic structure and as a cousin to the other basic equations of mathematical fluid dynamics,namely the incompressible Navier-Stokes and Euler equations.

    In this paper,we study a stochastic version of the PEsand develop techniques which may be viewed as a first step toward their numerical analysis.From the point of view of applications,this work is motivated by a plea from the geophysical community to further develop the theory of nonlinear stochastic partial differential equations(SPDEs for short)in a large scale fluid dynamics context and in general(see[63]).Indeed,in view of the many sources of uncertainty both physical and numerical which are typically encountered by the modeler,stochastic techniques are playing an increasingly central role in the study of geophysical fluid dynamics(see,e.g.,[9,23,45,52,55,59,62,75]and also[32]for a small sampling of this vast literature).

    The primitive equations trace their origins to the beginning of the 20th century with the seminal works of Bjerknes and Richardson[6,61]and have played a central role in the development of climate modeling and weather prediction since that time(see[56]).To the best of our knowledge,the development of the mathematical theory for the deterministic PEs began in the early 1990’s with a series of articles by Lions,Temam and Wang[46–48].This direction in mathematical geophysics is now a fairly well developed subject with results guaranteeing the global existence of weak solutions which are bounded in(see[47]),and the global existence and uniqueness of strong solutions,i.e.,solutions evolving continuously in(see[13,38–39,43]).Of course,these latter developments stand in striking contrast to the current state of the art for the Navier-Stokes equations as proving the global existence and uniqueness of strong solutions is tantamount to solving the famous Clay problem.For further background on the deterministic mathematical theory,see the recent surveys[60,64].

    Recently,significant efforts have been made to establish suitable analogues of the above(deterministic)mathematical results in a stochastic setting.In a series of works[15–16,24,27,30–31,35],the mathematical theory of strong,pathwise1Here pathwise refers to the fact that solutions are found relative to a prescribed driving noise.In this paper,we use the terms “pathwise” and “martingale” as opposed to the alternate terminology of“weak” and “strong”solutions to avoid confusion with the typical PDE terminology for which weak solutions are,roughly speaking,those inand strong solutions are those insolutions has been developed.These recent works more or less bring this aspect of the subject to the state of the art,that is they establish,in increasingly physically realistic settings,the global existence and uniqueness of solutions evolving continuously in

    Notwithstanding the above cited body of works,many aspects of the stochastic theory still need further consideration.In this paper,we develop existence results for weak solutions,which remain bounded in time only inThis is a direction which,to the best of our knowledge,remained unaddressed previously.Since such “weak solutions” are not expected to be unique,even in the deterministic setting,it is natural to work within the framework of martingale solutions.In other words,we consider below solutions which are weak in both the sense of PDE theory and stochastic analysis.

    One particular advantage of this weak-martingale setting is that it allows us to consider physical situations unattainable so far in the above cited works on strong(or strong-pathwise)solutions.From the deterministic point of view,we obtain results for the case of in homogenous,physically realistic boundary conditions.On the other hand,from the stochastic viewpoint,our results cover a very general class of state-dependent(multiplicative)noise structures.In particular,these noise terms may be interpreted in either the It? or Stratonovich sense.The latter Stratonovich interpretation of noiseisimportant as it may bemorerealistic in geophysical settings(see,e.g.,[37,57]for further details).Note that we develop our analysis in a slightly abstract setting which at once allows us to treat the PEs of the oceans,the atmosphere and the coupled oceanic/atmospheric system.2We have previously taken such an abstract approach in other work on the stochastic primitive equations(see[15]).There however our focus was on the local existence of strong,pathwise solutions and that framework was,by necessity,more restrictive with respect to domains,noise structures,etc.

    While the results established here take an important further step in the development of the analytical theory for the PEs,we believe that the main contribution of this article relates to numerical considerations.The approach below centers on an implicit Euler(i.e.,time discrete)scheme,and we choose this set-up mainly because it may be seen as a mathematical setting suitable for the development of tools needed for the numerical analysis of the stochastic PEs and other nonlinear SPDEs arising in fluid dynamics.Note that while discrete time approximation was previously employed in[14,17],these works treat hyperbolic type systems and only address the case of an additive noise.As such,a number of the techniques developed here,play a crucial role in a work related to the stability and consistency of a class of numerical schemes(both explicit and semi-implicit)for the 2D and 3D stochastic Navier-Stokes equations(see[33]).

    Let us now finally turn to sketch some of the main technical challenges and contributions of the article.In fact,the first main difficulty is to justify the validity of the implicit scheme on which our analysis centers.While classical arguments involving the Brouwer fixed point theorem can be used to establish the existence of sequences satisfying the implicit scheme,we crucially need that these sequences are adapted to the driving noise.To address this concern,we rely on a specifically chosen filtration and a suitable measurable selection theorem from[10](see also[11,41]).

    With suitable solutions to these mi-implicit scheme in hand,basic uniform estimates proceed analogously to the continuous time case with the use of martingale inequalities,etc.In contrast to previous works on Martingale solutions(see,e.g.,[4,15,25,34,51]),we circumvent the need for higher moments with suitable stopping time arguments.Another difficulty related to the concern that solutions are adapted appears when we associate continuous time processes with the discrete time schemes in pursuit of compactness and the passage to the limit.In contrast to the deterministic case(see[53,71]),we must introduce processes which are lagged by a time step.While these processes are indeed adapted,we obtain a time evolution equation with troublesome error terms.In turn,these error terms prevent us from addressing compactness directly from the equations and force us to carry out the compactness arguments for a series of interrelated processes.

    1.1 Organization of this pap er

    The exposition is organized as follows.In Section 2,we outline an abstract,functional analytic framework for the stochastic primitive equations(and related evolution systems)which may be seen as an “axiomatic”basis for the rest of the work.The section concludes by recalling the basic notion of Martingale solutions within the context of this framework.In Section 3,we introduce an implicit Euler scheme which discretizes the equations in time.The details of the existence of suitable solutions(adapted to the specific filtration)of this implicit scheme along with associated uniform estimates are given in Propositions 3.1 and 3.2,respectively.In Section 4,we study some continuous time processes associated with the implicit Euler scheme introduced in Section 3.Section 5 then outlines the compactness(tightness)arguments that allow us to pass to the limit and derive the existence of solutions from these approximating continuous time processes.Finally,Section 7 provides extended details connecting the abstract results that we just derived with the concrete example of the primitive equations of the oceans.In this section,we also provide a number of examples of possible types of nonlinear state dependent noises covered under the main abstract results.In the interest of making the manuscript as self-contained as possible,an Appendix(Section A)collects various technical tools used in the course of our analysis.

    After this work was completed,we heard of[3]which we regrettably overlooked.In this paper,the authors study the space and time discretization of the incompressible Navier-Stokes equations with multiplicative random forcing in space dimension 2 or 3.The space discretization of the equations is made by finite elements and the time discretization by an implicit Euler scheme.In this paper,we only perform discretization in time,also by an implicit Euler scheme.However,the issue of time and space discretization will bead dressed in a forthcoming paper[33].Note that[33]is still distinct from[3]because we also discuss in this paper the discretization of the Navier-Stokes equations by an explicit or semi-implicit scheme which raises issues of a.s.stability,a question not addressed in[3].

    We continue with some additional remarks and comparisons between[3]and the present paper,and leave to[33]some further comparisons of[3]with our work.

    (i)Regarding the equations considered,we study here a class of“abstract” fluid mechanics equations as in[16],and this class of equations covers the Navier-Stokes equations as well as the primitive equations of the atmosphere and the oceans(see,e.g.,[46–48]).[3]dealt only with the Navier-Stokes equations.Because of the difficulty of constructing divergence free finite elements,the authors of[3]chose to deal with weakly incompressible finite elements,using the antisymmetrized form of the nonlinear term introduced in[67–68]to overcome the difficulties arising from handling approximate functions which are not exactly divergence free(see[3,33]for further aspects of the spatial discretization).

    (ii)In[3],the authors construct martingale solutions to the 3D Navier-Stokes equations and pathwise solutions to the 2D Navier-Stokes equations,also called weak and strong solutions in the probabilistic sense.All solutions are weak solutions in the PDE sense that is correspond to L∞(L2)and L2(H1)solutions.In our case,the framework is general enough to include the 3D Navier-Stokes equations and therefore we only obtain martingale solutions;we do not specialize our results to the 2D case.

    (iii)The tools are generally the same in both articles:Existence of approximate solutions Un≈ U(n?t)by a fixed point method,energy a priori estimates,and compactness argument to pass to the limit.However,the construction of the approximate solutions Un≈ U(n?t),raises a delicate question of measurability which we fully address in this paper.We did not see how this issue of measurability is addressed or bypassed in[3].This issue of measurability was also overlooked in[14]to which[3]refers.The authors of this paper thank Debussche for helping them resolve this measurability difficulty.

    (iv)In[3],the authors derived estimates on higher moments after assuming that U0is deterministic,which implies that U0is uniformly bounded in the probability space and in turn makes the derivation of the higher moments estimate possible.However,we assumed that the initial data belongs to only L2in the probability space and thereby were forced to develop some techniques to overcome the lack of higher moment estimates when e.g.,establishing the compactness argument.

    (v)In both papers,the passage to the limit is based on the construction of auxiliary approximate processes.We use very different arguments than that in[3].However,it is not clear whether the methods are interchangeable in both circumstances,as again the lack of higher moment estimates in our case may matter,so much so that the more probabilistic approach of[3]may fail.Another difference is that,in 2D space,[3]provided the convergence to the unique solution using a monotonicity argument.This argument is inspired from the theory of montone operators of Minty and Browder[8,49](see also[7,44]for pseudo monotone operators).The argument was extended to the stochastic context in[50](see also[28,51]).However,this argument implies uniqueness and therefore it cannot be applied to the general framework that we study which includes the 3D Navier Stokes equations.

    This paper is dedicated to Haim Brézis on the occasion of his 70th birthday with admiration and friendship and(for RT)warm recollection of many years of interaction.

    2 The Abstract Problem Set-up

    We begin by describing the setting for the abstract evolution equation that we will study below(see(2.13)at the end of this section).As we note in the introduction,we take this point of view in order to systematically treat the existence of weak solutions to a class of geophysical fluids equations including but not limited to the example(7.1)–(7.4)developed below in Section 7.For further details about how to cast other related equations of geophysical fluid dynamics in the following abstract formulation,we refer the reader to[60]and the references therein.

    Throughout what follows,we fix a Gelfand-Lions inclusion of Hilbert spaces

    Each space is densely,continuously and compactly embedded in the next one.We denote the norms for H and V by|·|and ∥·∥,respectively,and the remaining spaces simply by e.g.When the context is clear,we denote the dual pairing betweenby

    2.1 Basic op erators

    We now outline the main elements,a collection of abstract operators,which we use to build the stochastic evolution(2.13)below.We suppose that the following are given.

    (1)A linear continuous operatorwhich defines a bilinear continuous formon V.We assume that a is coercive,i.e.,

    This term will typically capture the diffusive terms in the concrete equations:Molecular and eddy viscosity,diffusion of heat,salt,humidity,etc.3In previous works on the Stochastic PEs(see[15,30–31]),we required that this a is symmetric.In particular,such a symmetry was strongly used in these previous works so that we could apply the spectral theorem to the inverse of an associated operator A?1.This is not needed for the arguments presented here,and we therefore revert to the more general weak formulation of the PEs given in[60].

    (2)A second linear operator E continuouson both H and V;E defines a bilinear continuous form e(U,U?):=(EU,U?)on H(which is also continuous on V).We suppose furthermore that e is antisymmetric,that is,

    This term E appears in applications to account for the Coriolis(rotational)forces coming from the rotation of the earth.

    (3)A bilinear form B which continuously maps V×V intoB givesriseto an associated trilinear formwhich satisfies the estimates

    Moreover,we assume the antisymmetry property

    Note that,in particular,we may infer from(2.4)that

    Furthermore,from(2.4)–(2.5),we may assume that B is continuous from V ×V(2)into V′and satisfies

    Finally,we impose some additional technical convergence conditions on b.Firstly,we suppose that when Ukconverges weakly to U in V then,up to a subsequence k′,

    Similarly,we assume that if,for some T>0,

    then,again up to a subsequence k′,

    B accounts for the main nonlinear(convective)terms in the equations.

    (4)An externally given element ?.We consider ? to be random in general;it is specified only as a probability distribution on(0,∞;V′)subject to the second moment condition(2.17)given below.This term ? captures various inhomogeneous elements,i.e.,externally determined body forcings,boundary forcings,etc.

    In order to define the operators involving the“stochastic terms” in the equations,we consider an auxiliary space U,on which the underlying driving noise,a cylindrical Brownian motion W evolves(see Subsection 2.2).We suppose that U is a separable Hilbert space and useto denote the space of Hilbert-Schmidt operators frominto X,where,for example X=H,V or R.Sometimes,we abbreviate and write

    Returning to the list of operators,we suppose that we have defined the following.

    (1)A(possibly nonlinear)continuous mapWe suppose thatσ is uniformly sublinear,i.e.,

    where the constant c3>0 is independent of t∈ [0,∞).For economy of notation,we will frequently drop the dependence on t in the exposition below.We defineaccording tofor U,U?∈ H.The elementσ determines the structure of the(volumic)stochastic forcing applied to the equations.These stochastic terms typically appear to account for various sources of physical,empirical and numerical uncertainty as we described in the introduction.

    (2)A continuous map ξ:[0,∞)×H 7→ H which is subject to the uniform sublinear condition

    where c4>0 does not depend on t≥ 0.We defineby

    for U,U?∈ H.Weincludeξin the abstract formulation to allow,in particular,for the treatment of a class of Stratonovich noises; ξarises when we convert from a Stratonovich into an It? type noise.This term S therefore allows us to carry out the forthcoming analysis entirely within the It? framework(see Remarks 2.1,7.3 below).

    With the above abstract framework now in place,we may reduce the problem(7.1)–(7.4)below(and related equations)to studying the following abstract stochastic evolution equation in,namely,

    This system is to be interpreted in the It? sense which we recall immediately below in Subsection 2.2.

    Note that U0and ? in(7.1)are considered to be random in general.Indeed,since we are studying Martingale solutions to(2.13)where the underlying stochastic elements in the problem are considered as unknowns,we will specify U0and ? only as probability distributions on H and L2(0,T;V′)(see Definition 2.1 and Remark 2.1).Note also that,for brevity of notation,we sometimes write

    in the course of the exposition below.When the context is clear,we sometimes drop the dependence on t and simply write N(U).

    2.2 Some elements of stochastic analysis and abstract probability theory

    Of course,(2.13)is understood relative to a stochastic basisP,that is a filtered probability space with{Wk}k≥1,a sequence of independent standard 1D Brownian motions relative to Ft.Here we may define W on U by considering an associated orthonormal basis{ek}k≥1of U and takingW is thus a“cylindrical Brownian”motion evolving over U.

    Note that the embedding of U?U0is Hilbert-Schmidt.Moreover,using standard martingale arguments with the fact that each Wkis almost surely continuous,we have that,for almost every ω ∈ ?,W(ω)∈ C([0,T],U0).

    Since(2.13)is actually short hand for a stochastic integral equation,we next briefly recall some elements of the theory of It? stochastic integration in infinite dimensional spaces.We choose an arbitrary Hilbert space X and,as above,we use L2(U,X)to denote the collection of Hilbert-Schmidt operators from U into X.Given an X-valued predictable4For a given stochastic basis S,letΦ=?×[0,∞)and take G to be the sigma algebra generated by the sets of the formRecall that an X valued process U is called predictable(with respect to the stochastic basis S)if it is measurable from(Φ,G)into(X,B(X))where B(X)denotes the family of Borelian subsets of X.process G∈the(It?)stochastic integral

    is defined as an element inthe space of all X-valued square integrable martingales(see[58,Subsections 2.2–2.3]).For further details on the general theory of infinite-dimensional stochastic integration and stochastic evolution equations,we refer the reader to[19,58].

    Since we will be working in the setting of Martingale solutions,where the data in the problem(2.13)are specified only as a probability distribution(over an appropriate function space),it is convenient to introduce some further notations around Borel probability measures.Let(H,ρ)be a complete metric space and denote the family of Borel probability measures on H by Pr(H).Given a Borel measurable functionand an element μ ∈ Pr(H),we sometimes write μ(f)forwhen the associated integral makes sense.In particular,we write

    We review some basic properties related to convergence and compactness of subsets of Pr(H)in the Appendix below(see Section A.1).We refer the reader to[5]for an extended treatment of the general theory of probability measures on Polish spaces which include Hilbert spaces such as H and V.

    2.3 Definition of martingale solutions and statement of the main result

    We turn now to give a rigorous meaning for the so-called weak-martingale solutions to(2.13)which are defined as follows.

    Definition 2.1(Weak-Martingale Solutions)FixμU0,μ?Borel measures respectively on H andwith

    A weak-martingale solutionto(2.13)consists of a stochastic basisand processesand(defined relative toadapted toThis triplewill enjoy the following properties:

    (i)For every T>0,

    (ii)For every t>0 and each test function

    almost surely.

    (iii)Finally,andhave the same laws asμU0,μ?,i.e.,

    With this definition in hand,we now state one of the main results of the work as follows.

    Theorem 2.1LetμU0,μ?be a given pair of Borel measures on respectively H and∞;V′)which satisfy the moment conditions(2.17).Then,relative to this data,there exists a martingale solutionto(2.13)in the sense of Definition 2.1.

    Remark 2.1Depending on the structure ofσthe application of noise leads to a variety of different effects on the behavior of the solutions.In particular,σcan be chosen so that the noise either provides a damping or an exciting effect.It is therefore unsurprising that the structure of the stochastic terms in e.g.(7.1)remains a subject of ongoing debate among physicists and applied modelers.In any case,viewed as a proxy for physical and numerical uncertainty,the structure of the noise would be expected to vary by application.With this debate in mind we have therefore sought to treat a very general class of state-dependent noise structures inσ requiring only the sublinear condition(2.10).We have illustrated some interesting examples covered under this condition in Subsection 7.3 below.

    Actually,the Stratonovich interpretation of white noise driven forcing may often be more appropriate for applications in geophysics(see,e.g.,[37,57]for extended discussions on this connection).Note that although(2.13)is considered in ansense,an additional,state dependent drift termξis added to the equations which allows us to treat a class of Stratonovich noises with(2.13)via the standard “conversion formula” between It? and Stratonovich evolutions(see,e.g.,[1]and also Subsection 7.3 where we present one such example of Stratonovich forcing in detail).

    3 A Discrete Time Approximation Scheme

    We now describe in detail the semi-implicit Euler scheme,(3.3),which we use to approximate(2.13).This system is given rigorous meaning in Definition 3.1.We then recall a specific stochastic basis in Subsection 3.2 and establish the existence of solutions to(3.3)in Proposition 3.1 relative to this basis.We conclude this section by providing certain uniform bounds(energy estimates)independent of the time step of the discretization in Proposition 3.2.

    3.1 The implicit scheme

    Fix a stochastic basisand elements∞;V′)),U0∈ L2(?;H)whose distributions correspond to the externally given.For a given T>0 and any integer N,let

    along with the associated stochastic increments

    Using an implicit Euler time discretization scheme,we would then like to approximate(2.13)by considering sequencessatisfying

    infor n=1,···,N.For how to choose,see Remark 3.1.The termsare given by

    and the operatoris any approximation ofσwhich satisfies

    for every t≥0 and every U∈H.Additionally,we suppose that,for any t≥0,

    For the existence of such σN,see Remark 3.1.We write5The choice of a “time explicit” term in is needed to obtain the correctstochastic integral in the limit as?t→0.Actually,this adaptivity(measurability)concern also leads us to introduce the approximations ofσin(3.3)(see Remark 3.1,(4.6),(4.21)).Note that,as explained in this remark approximations ofσ satisfying(3.5)–(3.7)can always be found via an elementary functional-analytic construction.

    We make the notion of suitable solutions to(3.3)precise in the following definition.

    Definition 3.1We consider a stochastic basisGiven N ≥ 1 and an elementwhich ismeasurable and a process?=adapted to,we say that a sequenceis an admissible solution of the Euler Scheme(3.3),if

    (i)for eachandis Fnadapted,where Fn:=Ftn,n=0,···,N;

    (ii)every pairsatisfies

    almost surely for all U?∈V(2);

    (iii)for eachandsatisfy the “energy inequality”,almost surely on?:

    for n=1,···,N and where c1is the constant from(2.2).

    Remark 3.1At first glance the dependence on N in both the initial condition and the noise term involvingσmay seem strange.Indeed,in the deterministic setting,when we approximate(2.13)with(3.3),we would simply taketo be equal to the initially given U0for all N.Similarly,if we were to add deterministic sublinear terms analogous toσto the governing equations,no approximation as in(3.5)–(3.7)would be necessary.However,the situation is,in general,more complicated in the stochastic setting as we shall see in detail in Section 4,Proposition 4.1.This is essentially because we must construct continuous time processes from the’s which are adapted to a given filtration(see(4.6),(4.15)–(4.17)and(4.21)for specific details).

    For now let us describe how we can achieve suitable approximations in theand σN’s.

    (1)For a given initial probability distributions μU0,on H(withand having fixed a suitable stochastic basis and an element U0∈ L2(?;H),F0-measurable,with distributionwe then pick a sequencesuch thatin L2(?;H)but subject to the restriction given in(4.3)below.Such a sequence can be found with a simple density argument.Indeed,since V(2)is dense in H,we may initially approximate U0in L2(?,H)with a sequenceWe then define M(N)=max{M ≥ 1:and defineSinceapproximates U0in L2(?;H)while maintaining the constraint(4.3).

    (2)We may construct elements σNfrom σ satisfying(3.5)–(3.7)according to the following general functional analytic construction.For any U∈H,via Lax-Milgram we defineΨ(U)to be the unique solution in V of(Ψ(U),U?)=(U,U?)for all U?∈ V.Classically,Ψ is a compact,self-adjoint and injective linear operator on H.Thus,by the spectral theorem,we may find a complete orthonormal basis for H,{Φj}j≥1,which is made up of eigenfunctions ofΨ with a corresponding sequence of eigenvalues{γj}j≥1decreasing to zero.For any integer m,we let Pmto be the projection onto.Now choose a sequence mNincreasing to infinity but so thatIt is not hard to see that defined in this waysatisfies the requirements given in(3.5)–(3.7).

    3.2 Existence of the

    While the existence for a.e.ω∈? of solutions to(3.3)satisfying(3.9)follows along arguments similar to those found in[60,Lemma 2.3],some care is required to demonstrate the existence of sequenceswhich are adapted to the underlying stochastic basis.For this complication,we will make use of a“measurable selection theorem”(see Theorem A.2)from[10](see also the related earlier works[11,41]).In order to apply this result,we use a specific stochastic basis defined around the canonical Wiener space whose definition we recall next.

    3.2.1 The Wiener measure and its filtration

    We recall the canonical Wiener space as follows(see[42]for further details).Let

    equipped with the Borelσ-algebra denoted as G.We equip(?,G)with the Wiener measure P.6Using the orthonormal basis{e k}k≥1 of U,P is obtained as the product of the independent Wiener measures each one defined on C([0,T];R).Then the evaluation map W(ω,t):= ω(t),ω ∈ ?,t∈ [0,T],is a cylindrical Wiener process on U0.The filtration is given by Gtdefined as follows:

    the completion of the sigma algebra generated by the W(s)for s∈[0,t]with respect to P.Combining these elements SG=(?,G,{Gt}t≥0,P,W)gives a stochastic basis suitable for applying Theorem A.2.

    3.2.2 Existence of the’s adapted to G t n

    Proposition 3.1Suppose that

    where c4is the constant arising in(2.11).Consider the stochastic basis SGdefined as in Subsection 3.2,an N ≥ N0,and an elementwhich is G0-measurable and a process ?= ?(t)∈ L2(?;L2(0,T;V′))measurable with respect to the sigma algebra generated by the W(s)for s∈[0,t].Then there exists a sequencewhich is an admissible solution to the Euler scheme(3.3)in the sense of Definition 3.1.

    The rest of this subsection is devoted to the proof of Proposition 3.1.Below we will construct the sequenceiteratively starting frombut we first need to take the preliminary step of establishing the existence of a certain Borel measurable mapwhich is used at the heart of this construction.

    We define the continuous mapaccording to

    and,for each t∈[0,T]and F ∈V′we set

    Using this family of sets defined by(3.12),we now establish the following lemma.

    Lemma 3.1There exists a mapwhich is universally Radon measurable(Radon measurable for every Radon measure on(0,T)×V′),such that for every t∈ (0,T)and every F ∈V′,U:= Γ(t,F)∈ Λ(t,F).

    ProofWe establish the existence of the desired Γ by showing that Λ satisfies the conditions of Theorem A.2.More precisely,we need to verify that7To apply Theorem A.2,we actually would like to defineΛon the Banach space R×V′.For this purpose,we may simply takeΛ(t,F)=Λ(T,F)when t>T,and when t<0 we letΛ(t,F)=Λ(0,F).

    (i)for each t∈ [0,T],F ∈ V′,the setΛ(t,F)is non-empty,

    (ii)Λ(t,F)is closed.In other words,we need to show that,given any sequences

    such that,for every n,

    we have

    Observe that,for any Umof this form,using(2.2)–(2.3),(2.5)and(2.11),we estimate

    We next seek bounds on the resulting sequence of Um’s in V independent of m.Starting from(3.13),we find that

    Using once again the standing assumption(3.10),we have that Umis bounded in V independently of m.Passing to a subsequence as needed and using that V is compactly embedded in H,we infer the existence of an element U such thatweakly in V and strongly in H.

    Returning to(3.14)and using the lower semicontinuity of weakly convergent sequences,we obtain thatTo show that U satisfiesfor everywe simply invoke(2.8)for B and the other continuity assumptions on A,E andξ,and obtain this identity forfor each k≥ 1.By linearity and density,we therefore infer the identify for arbitrary.With this we now have established(i).The second item,(ii),to show thatΛis closed,follows immediately from the continuity of G from[0,T]×V intoand the continuity ofξfrom[0,T]×H into H.The proof of Lemma 3.1 is therefore complete.

    Construction of an adapted solution

    Step 1We will build the desired sequenceinductively as follows:

    withmeasurable for V equipped with B(V)and C([0,tn];U0)equipped with Gn:=Gtn(defined as in Subsection 3.2).

    Suppose that we have obtainedfor some n ≥ 2.Since Gn?1is the completion ofwith respect to the Wiener measure8We observe that the sigma algebra generated by the W(s)for s∈(0,t)is justwhereis the mapping(see[42]).is P-measurable.Now we defineby setting

    Then we can define

    SinceσNis a continuous map,clearlyis a continuous map.Moreover,Γ is universally Radon measurable thanks to Lemma 3.1,hence Corollary A.1 applies and we infer thatχis universally Radon measurable from the Borel sigma algebra onto the Borel sigma algebra on V.

    Since?= ?(t)is a process assumed to be measurable with respect to the sigma algebra generated by the W(s)for s ∈ [0,t],is measurable with respect to the sigma algebra generated by the W(s)for s∈[0,tn]thanks to(3.4).Hence by Theorem A.1 in the appendix with X as?,(Y,M)asψ asas V,we see that there exists a functionwhich is Borel measurable,such that

    From(3.17)–(3.18),we infer

    Sinceandare P-measurable,and κ is universally Radon measurable,Theorem A.3 applies and we infer thatis P-measurable,that isis measurable with respect to Gn.

    Step 2We infer thatis measurable with respect to Gnas desired.

    Observe moreover that,according to Lemma 3.1(see(3.12)),,for everyandwhich is to say thatandsatisfy(3.3)and(3.9).

    It remains to show thatWe start from(3.9),now established forandand use the elementary identityand obtain

    almost surely.To address the terms involving?,we have that(see(3.4))

    where we defineaccording to

    For the terms involving s defined as in(2.12),we simply infer from(2.11)

    With H?lder’s inequality,we find

    Then using that gNis linear in its second argument,we have

    Using these observations forand s,we rearrange and infer that,up to a set of measure zero,

    Using(2.10),(3.6)and thatis Gn?1-measurable,in L2(?;H),we have

    From this observation,(3.25)and(3.10),we infer

    which implies that,as needed.

    We have thus established the iterative step in the construction of.The base case,n=1,is established in an identical fashion to the iterative steps.The proof of Proposition 3.1 is now complete.

    Remark 3.2Although necessary for the establishment of the existence of the’s in Proposition 3.1,it is not necessary to assume the underlying stochastic basis to be SG(defined in Subsection 3.2)in the results through out Subsection 3.3 to Subsection 5.1.The reason is that these results are true whenever such’s defined as in Definition 3.1 exist.In other words they are independent of the choice of the underlying stochastic basis.Similarly,it is not necessary at this point to assume that U0and ? have laws which coincide with those of the externally givenμU0 andμ?for these results.

    However,it is necessary that we resume these assumptions of SG,μU0and μ?starting in Subsection 5.2.

    3.3 Uniform “energy” estimates for the

    Starting from(3.9)we next determine certain uniform bounds,independent of N,for(suitable)sequencessatisfying(3.3)as follows.

    Proposition 3.2Let

    where c3and c4are from(2.10)and(2.11),respectively.Letbe the given stochastic basis and assume thatis measurable with respect to Ft.For each N ≥N1,we assume thatmeasurable and such that

    Then for each N ≥ N1,consider the sequenceswhich satisfy(3.3)starting fromand relative to?in the sense of Definition 3.1.Then

    ProofThe starting point for the estimates leading to(3.28)is of course(3.9)and from this inequality,we can use the same proof as in Proposition 3.1 to obtain(3.25).In order to make suitable estimates for the final two terms in(3.25),we need to take advantage of some martingale structure in the terms involving σN.For any 1≤m≤n≤N,we define the stochastic processes

    Summing(3.25)for 1≤m≤n=k≤l≤N,we find

    Sinceis adapted to Fn:=Ftn,it is easy to see thatis a martingale relative towithWe would like to apply a discrete version of the Burkholder-Davis-Gundy inequality,recalled here as in Lemma 3.2 to obtain estimates forUnfortunately,it is not clear thatis square integrable,so we have to apply a localization argument to make proper use of this inequality.For any K>0,we define the stopping times

    Since

    we have thatalmost surely asClearlyis a square-integrable martingale.For the moment,let us recall a discrete analogue of the Burkholder-Davis-Gundy inequality.This result and other related martingale inequalities can be found in e.g.[22].

    Lemma 3.2Assume that{Mn}n≥0is a(discrete)martingale on a Hilbert space H(with norm|·|),relative to a given filtrationWe assume,additionally that M0≡ 0 and thatfor all n≥0.Then,for any q≥1 and any n≥1,

    where cqis a universal positive constant depending only on q9We may often determine c q in(3.31)explicitly,and in particular,we have that c1=3.(which is independent of n and{Mm}m≥0),and Anis the quadratic variation defined by

    Hence with the observation thatis-measurable,we compute the quadratic variation ofin view of(3.32)as follows:

    Thus,by Lemma 3.2,(2.10)and(3.6),we infer

    Hence,letting,we have,by the monotone convergence theorem,

    On the other hand,sinceis adapted to Fn,given the condition(2.10)onσand(3.6),we infer that

    We now use(3.33)–(3.34)with(3.30)and infer that

    Rearranging it,we find that

    for the constantwhich in particular depends only on c3,c4.Thus,subject to the condition

    we have

    whereThus,by iterating this inequality and noting from(3.21)that

    we finally conclude that

    Note carefully that,in view of(3.36),we need not iterate(3.37)more than,say,times to obtain(3.38).10Indeed,for N≥N 1,let N(N)be the minimum number of iterations of(3.37),subject to the constraint(3.36),which are needed to establish(3.38).Take F(N)to be the“fraction of the time interval that can be covered at each step”,namely, where the last inequality follows from the standing assumption(3.26).Since N(N)F(N)≤2,we finally estimate Here smallest integer that is larger than or equal to p.As such,we may takewhich,crucially,is independent of N.

    We now return to(3.30).With(3.34),we infer

    where we can takeAs such,(3.38)–(3.39)with(3.27)imply(3.28),completing the proof of Proposition 3.2.

    4 Continuous Time Approximations and Uniform Bounds

    In this section,we detail how the sequencesdefined in the sense of Definition 3.1 may be used to define continuous time processes that approximate(2.13).The details of establishing the compactness of the associated sequences of probability laws and of the passage to the limit are given further on in Section 5.

    We now fix sequencessatisfying(3.3)in the sense of Definition 3.1.For N≥N1,with N1as in(3.26),let

    Of course,we do not have any time derivatives of the UN’s(even fractional in time)as are typically needed for compactness.Furthermore,we would like to be able to associate an approximate stochastic equation for(2.13)with theseFor these dual concerns,we introduce further stochastic processes and consider

    Remark 4.1The processes UNandare slightly different than those typically used in the deterministic case(see,e.g.,[71]).Actually,these processes are essentially their deterministic analoguese valuated at time t by their value at time t??t.With this choice,we crucially obtain processes which are adapted toNot surprisingly however the present definitions ofleads to bothersome error terms in(4.6)below.In turn these error terms dictate the additional convergences inσand U0when we initially defined the discrete scheme(3.3)(see(3.5)–(3.7)and Remark 3.1).These error terms also complicate compactness arguments further in Section 5(see Remark 4.2).

    The rest of this section is now devoted to proving the following desirable properties of UNand

    Proposition 4.1Letbe a stochastic basis,and let N1be as in(3.26)in Proposition 3.2.Consider a sequencebounded in L2(?,H)independent of N,with-measurable for each N and such that

    for a constant c>0,independent of N.11The constraint(4.3)is necessary for(4.4)–(4.7).This is not a serious restriction when we pass to the limit in Section 5.As we described above in Remark 3.1,for any given U 0∈ L 2(?;H)we may obtain a sequenceapproximating U 0 which maintains(4.3).Suppose that we also have defined a process?=?(t) ∈ L2(?;L2(0,T;V′))adapted to

    For each N≥N1,we consider sequenceswhich satisfy(3.3)starting fromin the sense of Definition 3.1.Once these sequencesexist,then we define the continuous time processesaccording to(4.1)and(4.2),respectively.Then,

    (i)for eachand-adapted and

    Moreover,we have that

    (ii)UNandsatisfy a.s.and for every t≥0,

    subject to error termswhich are defined explicitly in(4.15)–(4.16)below.

    (iii)These error termssatisfy

    respectively,and moreover,

    We proceed to prove Proposition 4.1 in a series of subsections below.The proof of(i)is essentially a direct application of Proposition 3.2,and we provide the details in the subsection immediately following.In Subsection 4.2,we provide the details of the derivation of(4.6)and in particular explain the origin of the error terms.The final Subsection 4.3 provides details of the estimates for these error terms which lead to(4.7)–(4.9).

    Remark 4.2It is not straightforward to obtain fractional in time estimates forfrom(4.6)in view of the error terms which have a rather complicated structure(see(4.15)–(4.16)).As such,we cannot establish sufficient compactness for the sequencedirectly to facilitate the passage to the limit.For this reason,we choose to introduce additional continuous time processes in Section 5 below.An alternate approach will be presented later on in the related work[33].

    4.1 Uniform bound s and clustering

    It is clear from(4.1)that UNis{Ft}t≥0-adapted and that

    Thus,since(3.27)holds,we have the uniform bound(3.28)from Proposition 3.2,and we immediately infer that

    with the integer N1appearing in(3.26).

    As the UNabove,it is easy to see from(4.2)thatis adapted to{Ft}t≥0,and thatis adapted to Fn(=Ftn).Furthermore,direct calculations show that

    Using(4.11),similarly to[71],we compute that

    We thus infer(4.5)directly from this observation and(3.28).Based on similar considerations,we also have

    Thus,once again due to(4.3)and(3.28),we finally have

    With(4.10)and(4.12),we have now established the first item in Proposition 4.1.

    4.2 The ap proximate stochastic evolution systems

    We next derive the equation(4.6)relating UNandgiving explicit expressions forWe observe that,almost surely and for almost every t≥ 0(in fact for every

    where χ(t1,t2)denotes the indicator function of(t1,t2).Recall thatand letin other words,we takesuch that

    Working from(4.13)and(3.3),we therefore compute

    where the “error terms”,,are defined as

    and

    respectively.To understand the origin of these error terms,we observe that

    Moreover,using the definition of thein(3.4),we have

    On the other hand,for the error termsinvolving σNin(4.16),we compute

    4.3 The estimates for the error terms

    We next proceed to make estimates on the error termsandas desired in(4.7),(4.9).Perusing(4.15),we begin with estimates forInvoking the bounds provided by(2.7)along with the continuity properties of the other operators making up N in(2.14)defined in Subsection 2.1,we have

    As such,in view of the standing condition(4.3)(see Remark 3.1),we conclude that

    Forwe estimate in L2(0,T;V′)

    In summary,we have

    and so we conclude(4.7)from(4.17)–(4.18).

    We next turn to make estimates forWe begin with estimates in L2(0,T;H).Forwe observe with(2.10)and(3.6)(see(3.34))that

    and infer from(3.28)in Proposition 3.2 that

    On the other hand,with the It? isometry and another application of(2.10)and(3.6),we have

    so that

    By combining(4.19)–(4.20),we obtain(4.8).

    We turn now to establishing the uniform bounds announced in(4.9).Estimates similar to those leading to(4.19)–(4.20),but which instead make use of the condition(3.5),yield bounds in L2(0,T;V),namely,

    and similarly

    so that,taken together we infer that

    Finally,we supply a bound forin L∞(0,T;H).Forwe observe with(2.10),(3.6)that

    To estimatewe use Doob’s inequality and(2.10)to infer

    With these bounds and(3.28),we conclude that

    In turn,(4.21)–(4.22)directly imply(4.9),and so the proof of Proposition 4.1 is now complete.

    5 Compactness and the Passage to the Limit

    In this section,we detail the compactness arguments that we use to prove the existence of martingale solutions of(2.13)using the processes UNanddefined in the previous section.As it is not clear how to obtain compactness directly from(see Remark 4.2),we must introduce further processes to achieve this end.

    Recalling(4.1)–(4.2),(4.15)–(4.16),we define

    and then consider the associated probability measures

    Notice that,due to Proposition 4.1,are defined on the space X:=L2(0,T;H).Regarding the elements,we observe that,as a consequence of(4.6),

    As a result of this identity and Proposition 4.1,the elementsmay be regarded as measures on the space

    We will show below that μNandconverge weakly to a common measure μ and then make careful usage of the Skorohod embedding theorem to pass to the limit in(5.3)on a new stochastic basis.The former compactness arguments,which rely on the intermediate measureswill be carried out in the next subsection and the details of the Skorohod embedding will be discussed in Subsection 5.2 further on.

    5.1 Tightness arguments

    In this section,we will establish the following compactness properties of theand

    Proposition 5.1The assumptions are precisely those in Proposition 4.1.Defineandaccording to(4.1)and(5.1)and where N1is as in(3.26).Letbe the associated Borel measures on

    defined according to(5.2).Then,there exists a Borel measure μ onsuch that,up to a subsequence,12We recall the notion of weak compactness of probability measures along with the equivalent notion of tightness in Appendix(see Section A.1).

    The rest of this subsection is devoted to the proof of Proposition 5.1.We proceed as follows:First we show thatis tight(see Appendix A.1)in L2(0,T;H)by employing a suitable variant of the Aubin-Lions compactness theorem which we establish in Proposition A.4 below.We next show thatis tight in C([0,T];via an Arzelá-Ascoli type compact embedding from[25,70].We finally employ the estimates(4.5),(4.7)along with the general convergence results recalled in Lemma A.1 to finally infer(5.4)–(5.5).

    5.1.1 Tightness for in L 2(0,T;H)

    With the aid of Proposition A.4,we identify some compact subsets of X=L2(0,T;H)that,in conjunction with suitable estimates(see(5.10)–(5.13)immediately below)are used to establish the tightness ofin X.For U ∈ X,n>0,define

    and,for each R>0,consider

    It is not hard to show that each set BRis a closed subset of X.Perusing(5.6),it is clear that the condition(A.4)holds uniformly for elements in BR.Thus,as a consequence of Proposition A.4(ii),these sets BRare compact in X=L2(0,T;H)for each R>0.

    Now,for each R>0,we have

    As a consequence of(4.4),(4.9)and(5.1),we have

    for some constant c independent of N.

    with

    To addresswe observe,with(2.6)and the standing assumptions on the operators that make up N in(2.14),that for any U∈V,

    Furthermore,it is clear from(3.4)and H?lder’s inequality that,a.s.

    Combining these observations,we infer that,a.s.

    For the term,we estimate,for 0≤θ≤δ,

    where the second line follows from Doob’s inequality and the standing assumptions(2.10)on σand(3.6)onσN:

    The estimates(5.12)–(5.13)allow the second term in(5.8)to be treated as follows.Observe that according to(5.6)and(5.10),we have

    For the first term,we observe with(5.12)that

    Regarding the second term,we simply bound

    so that forρ>0,sufficiently large,

    We finally conclude that

    Combining(5.8)–(5.9)and(5.16),we now conclude that(see Appendix A.1)

    5.1.2 Tightness for

    We next show thatis tight inFor this purpose,we make appropriate usage of a compact embedding from[25](see also[70]).Let us fix anysuch thatαp>1.According to[25],

    that is,the embeddings are continuous and compact.We now define

    for any R>0.With(5.18),it is clear that BRis compact infor every R>0.Observe moreover that,in view of(5.3),

    and thus that

    Hence we will infer thatis tight inif we can show thatconverge uniformly in N to zero as R↑∞.

    Forwe estimate,with(5.11),

    Thus we find(see(5.15))

    We turn toFor this purpose,let us define for any R>0 the stopping times

    UsingτR,we now estimate with the Chebyshev inequality that

    Now in order to treat this final stochastic integral term,we recall the following generalization of the Burkholder-Davis-Gundy inequality from[25]:For a given Hilbert space X,p≥2 andwe have for all X-valued predictable

    which holds with a constant c depending only onαand p.Continuing now from(5.21),we have

    Combining the estimates(5.20),(5.22)with(4.4),we finally conclude

    and hence infer that

    Remark 5.1Let us observe that the tightness bounds forcould be carried out differently if we had available,for example,the uniform bounds on “higher moments” like

    or equivalently that

    Indeed,in numerous other previous works related to stochastic fluids equations(see,e.g.,[4,15,25,34,51])estimates analogous to(5.25)are established essentially via It?’s lemma in order to achieve tightness in the probability laws associated to a regularization scheme.

    In the current situation,instead due to the way we carry out the estimates in(5.15),(5.21)–(5.22),we have adopted a different approach,namely,we establish tightness(compactness)estimates without recourse to such higher moment estimates.

    A different method using higher moments will be shown in the related work[33].

    5.1.3 Cauchy arguments and conclusions

    With(5.17)and(5.23)now in hand,it is then simply a matter of collecting the various convergences above to complete the proof of Proposition 5.1.

    By making use of Prohorov’s theorem(see Section A.1)with(5.17),we infer the existence of a probability measure μ such that,up to a subsequence,

    Due to(5.1)with(4.5)and(4.8),it is clear thatconverges to zero in X=L2(0,T;H)and hence in L2(0,T;V′)a.s.Hence,by now invoking(4.7)and referring back once more to(5.1),we have thatconverges to zero inThus,invoking Lemma A.1,again up to a subsequence,we conclude that

    In particular,this is the first desired convergence for(5.4).On the other hand,invoking Prohorov’s theorem with(5.23)and the convergence just established forin L2(0,T;V′),we see thatis tight inBy Prohorov’s theorem in the other direction and passing to a further subsequence as needed,we have

    Since,clearly,,this yields the second desired item(5.5).The proof of Proposition 5.1 is therefore complete.

    5.2 Proof of Theorem 2.1 conclusion:Almost sure convergence and the passage to the limit on the Skorokhod basis

    We now have all of the ingredients to finally prove the main results of this article,namely Theorem 2.1.Suppose that we are givenandaccording to the conditions specified in Definition 2.1.As mentioned in Remark 3.2,now it is necessary to introduce the stochastic basis SG(defined as in Subsection 3.2),an element U0which is G0measurable and a process?= ?(t)measurable with respect to the sigma algebra generated by the W(s)for s ∈ [0,t],13Note that since the sigma algebra generated by the W(s)for s∈[0,t])is the smallest respect to which W(t)is measurable,?(t)is adapted to{F t}t≥0,and hence all the previous results apply.whose laws coincide with those ofμU0,μ?.Thus Proposition 3.1 applies,and we obtain the existence of theadapted to Gtn.

    We then approximate U0∈ L2(?;H)with a sequence of elementswhich maintains the bound(4.3)as described in Remark 3.1 above.Proposition 4.1 applies,and hence we can use this sequence,the process ?,and the sequenceto define processesaccording to(4.1)and(5.1),respectively(N1is given by(3.26)).In order to pass to the limit in the associated evolution equation(5.3),we consider the product measures

    which are defined on the space

    where,as above,and U0is defined as in Subsection 2.2,(2.15).By invoking Proposition 5.1,we have that(passing to a subsequences as needed)μN? μ on X andon Y,whereμNandare defined as in(5.2).It follows,again up to passing to a subsequence,thatνNconverges weakly to a measureνon Z(defined in(5.27)).Furthermore,recalling(5.1)and making use of(4.5),(4.7)–(4.8),it is not hard to see that

    Thus,by making use of the Skorokhod embedding theorem(see Section A.1),we obtain,relative to a new probability space,a sequence of random variables

    Moreover,the uniform bounds forfrom Proposition 4.1,(4.4)imply that in addition to(5.28),we also have

    Following a procedure very similar to[4],we may now show thatis a cylindrical Brownian motion relative to the filtrationdefined as the sigma algebra generated byfor s≤t and thatsatisfies(5.3)on the“Skorokhod space”viz.

    Using the convergences in(5.28)–(5.29)with(5.30)it is standard14Note that,in particular,the stochastic terms involvingσN(U N)converge due to(3.7).to show thatsatisfies(2.18)–(2.20)relative to the stochastic basis,whereis defined as the sigma algebra generated by thefor s≤t andTherefore,is a martingale solution to(2.13)relative toμU0,μ?in the sense of Definition 2.1,and the proof of Theorem 2.1 is complete.

    6 Convergence of the Euler Scheme

    We conclude by reinterpreting from the point of view of numerical analysis,the study above as a result of convergence for the Euler scheme(3.3).

    Theorem 6.1We assume given μU0∈ Pr(H)andaccording to Definition 2.1.We also assume given the stochastic basis SG(defined as in Subsection 3.2),an element U0which is G0measurable and a process ?= ?(t)measurable with respect to the sigma algebra generated by the W(s)for s ∈ [0,t],whose laws coincide with those of μU0,μ?.Let a sequences of elementsapproximate U0∈ L2(?;H)as described in Remark 3.1.Then the processes{UN}N≥N1defined according to(4.1)(N1is given by(3.26))adapted to{Gt}t≥0exist.

    Moreover,the family{μN}of probability laws of{UN},is weakly compact over the phase spaceand hence converges weakly to a probability measure μ on the same phase space up to a subsequence.Furthermore,there exists a probability spaceand a subsequence of random vectorswith values insuch that

    (i)have the same probability distribution as(UNk,?,W).

    (ii)converges almost surely asin the topology of Z1,to an elementParticularly,wherehas the probability distributionμ.

    ProofThe existence offollows directly from the existence of theproven in Proposition 3.1.(i)and(ii)follow from the Skorokhod embedding theorem(see Section A.1)as shown in Subsection 5.2.

    7 Applications for Equations in Geophysical Fluid Dynamics

    In this section,we apply the above framework culminating in Theorems 2.1 and 6.1 to a stochastic version of the primitive equations.Our presentation here will focus on the case of the equations of the oceans.Note however that the abstract setting introduced above is equally well suited to derive results for analogous systems for the atmosphere or for the coupled oceanicatmospheric system(COA for short).15Via a suitable change of variables,the dynamical equations for the compressible gases which constitute the earth’s atmosphere may be shown to take a mathematical form essentially similar to the incompressible equations for the oceans.We refer the interested reader to[60]for further details on these other interesting situations.

    7.1 The oceans equations

    The stochastic primitive equations of the oceans take the form

    Here,U:=(v,T,S)=(u,v,T,S);v,T,S,p,ρrepresent the horizontal velocity,temperature,salinity,pressure and density of the fluid under consideration,respectively;μv,νv,μT,νT,μS,νSare positive coefficients which account for the eddy and molecular diffusivities(viscosity)in the equations for v,T and S.The terms Fv,FT,FSare volumic sources of momentum,heat and salt which are zero in idealized situations but which we consider to be random in general.

    The state dependent stochastic terms are driven by independent Gaussian white noise processeswhich are formally delta correlated in time.The stochastic terms may be written in the expansion

    where the elementsare independent 1D white(in time)noise processes.We may interpret the multiplication in(7.2)in either the It? or the Stratonovich sense;as we detail in one example below that the classical correspondence between theand Stratonovich systems allows us to treat both situations within the framework of the It? evolution(2.13).We will describe some physically interesting configurations of these “stochastic terms” in detail below in Subsection 7.3.

    The operatorsare the horizontal Laplacian and the gradient operator,respectively.Herethe operator?vcapturespart of the convective(material)derivative and is defined according to

    Remark 7.1As given,the model(7.1),expresses the equations for oceanic flows in the“beta-plane approximation”,that is to say we make use of the fact that the earth is locally flat.This setting is suitable for regional studies,and we will focus on this case for the simplicity of presentation.With suitable adjustments to the definition of the operators?,?,?vand to the domain introduced below we could consider the evolutions in the full spherical geometry of the earth.We refer to[47](and also to[60])for further details on how to cast a global circulation model in the form of(2.13).

    7.1.1 Domain and boundary conditions

    The evolution(7.1)takes place on a bounded domain M?R3which we define as follows.Fix a bounded,open domainΓi? R2with sufficiently smooth boundary(C3,say);Γirepresents the surface of the ocean in the region under consideration.We suppose that we have defined a“depth”function h=h(x,y):Γi→ R which is at least C2and is subject to the restrictionWith these ingredients,we then let

    The boundary ?M of M,is divided into its top Γi,lateralΓland bottom Γbboundaries.We denote the outward unit normal to?M by n and the normal toΓlin R2by nH.

    Wenext prescribe the following,physically realistic boundary conditions for(7.1)considered in M(see,e.g.,[60]for further details).OnΓiwe suppose

    where αv,αTare fixed positive constants,and τv,va,Taare in general random and nonconstant in space and time.Physically speaking,the first two equations in(7.4)account for a boundary layer model,where va,Tarepresent the values for velocity and temperature of the atmosphere at the surface of the oceans,respectively;τvaccounts for the shear of the wind.

    At the bottom of the oceanΓb,we take

    Finally for the lateral boundaryΓl,

    Note that,in view of the Neumann(no-flux)boundary conditions imposed on S in(7.4)–(7.6),there is no loss in generality in assuming

    (see[60]for further details).Finally,(7.1)–(7.7)are supplemented with initial conditions for v,T and S,that is,

    7.1.2 A reformulation of the equations

    Starting from the incompressibility condition,(7.1c)and the hydrostatic equation(7.1b),we may derive an equivalent form for(7.1)as follows:

    This reformulation is desirable as,in particular,it is more suitable for the typical functional setting of the equations which we describe next.The unknowns and parameters in the equations are precisely those given above immediately after(7.1).Of course,(7.9)is subject to the same initial and boundary conditions as in(7.1),namely(7.4)–(7.8).For further details concerning the equivalence of(7.9)and(7.1)(see[60]).

    7.2 The functional setting and connections with the abstract framework

    We now proceed to introduce the basic function spaces associated with the primitive equations(7.9)(equivalently(7.1)),and then introduce and explain the variational formulation of the various terms in equation connecting them with the abstract assumptions laid out above in Section 2.

    7.2.1 Basic function spaces

    To begin,we define the smooth test functions

    We now take H to be the closure of V in L2(M)4or,equivalently,H:=H1×H2,which is

    On H,it is convenient to define the inner product and norm according to

    The constants KT,KS>0,which are introduced for coercivity in the principal linear terms in the equations,are chosen in order to fulfill(2.2)for(7.14)below.We defineΠto be the orthogonal(Leray-type)projection from L2(M)4onto H.

    We shall next define the H1type space V=V1×V2,which is

    We endow V with the inner product and norm

    where

    From(7.11)–(7.12),we may deduce the Poincaré type inequality|U|≤ c∥U∥ for every U ∈ V.This justifies taking∥·∥as the norm for V(which is equivalent to the H1norm).Finally,we define

    and simply endow V(2)and V(3)with the H2(M)and H3(M)norms,respectively.Let V′(resp.be the dual of V(resp.V(2),V(3))relative to the H inner product.

    It is clear with the Rellich-Kondrachov theorem and standard facts about Hilbert spaces that the spaces introduced in(7.10)–(7.13)provide a suitable Gelfand-Lions inclusion as desired for(2.1).On this functional basis we now turn to describe the variational form of(7.9).

    7.2.2 The variational form of the equations

    To capture most of the linear structure in(7.9),we define the operator A as a continuous linear map from V to V′via the bilinear form

    We observe that if KT,KSin(7.12)are chosen sufficiently large,then a is coercive,namely,it satisfies the condition required by(2.2).

    where

    To capture the rotation(Coriolis)term in(7.9a),we define E:H→H via

    Note carefully that a,e and b satisfy the conditions imposed in Subsection 2.1 which we used in the abstract result Theorem 2.1.The in homogenous terms in(7.9)are given by the element ? defined according to

    Note that va,τv,Ta,which represent the velocity,shear force of the wind and the temperature at the surface of ocean,have significant uncertainties and should thus be considered to have a random component in practice.

    7.3 Some stochastic forcing regimes

    It remains to complete the connection between(7.1)and(2.13)by describing various physically interesting scenarios forWe connect these“concrete descriptions”with the terms σandξin the abstract equation(2.13)(or equivalently to g,s in(2.19)).We consider three situations in detail below.In each case,we describe how to defineσUappearing in(7.9),and we then take

    7.3.1 Additive noise

    The most classical case is to consider an additive noise,where we suppose thatσUis independent of U=(v,T,S).In other wordsFor(2.10)to be satisfied,we would require that

    Note that since the It? and Stratonovich interpretations of(7.2)coincide in the additive case,we may takeξ≡0 so that(2.11)is automatically satisfied.

    We also observe that in this case we may give an explicit(if formal)characterization of the space-time correlation structure of the noise

    where the correlation kernel K is given by

    Remark 7.2Given the condition(7.18),the case of space-time white noise is ruled out under our framework.Of course such a space-time white noise is very degenerate in space(not even defined inand so such a situation is far from reach due to the highly nonlinear character of the PEs.Similar remarks apply to the 3D stochastic Navier-Stokes equations,but see[18]for the 2-D case.

    7.3.2 Nemytskii type op erators

    We next consider stochastic forcings of transformations of the unknown U as follows.Letand suppose,for simplicity,thatΨ is smooth.We denote the partial derivatives ofΨ with respect to the v,T,S variables by ?vΨ,?TΨ,?SΨ respectively and the gradient by?UΨ.Take a sequence of smooth functionsαk= αk(x):M → R and define

    We may formally interpretwhere

    (1)is a white in time Gaussian process with the spatial-temporal correction structure

    (2)The“multiplication”Ψ(U)andmay be taken in either the It? or the Stratonovich sense.

    We now connect(7.20)to(2.13)in theor the Stratonovich situations in turn illustrating conditions on Ψ and the αk’s guarantee that(2.10)holds and in the Stratonovich case that(2.11)holds.

    The caseSuppose that

    and for the elementsαk,we suppose that

    The Stratonovich caseIf we understand the multiplicationΨ(U)˙ηin the Strantonovich sense,then we may convert back to an It? type evolution according to

    where

    Onecan refer to,e.g.,[1,40]for further details on this conversion formula.Under the additional assumption

    we defineξU(U):=Πξ(U)for any U ∈H.It is clear thatξsatisfies(2.11).

    Remark 7.3We note here that the relationship(7.23)is,for now,only formal;we prove the existence of martingale solutions to the system that results from a formal application of this conversion formula(see,e.g.,[1,40]).We leave the rigorous justification of(7.23)and the related issues of an approximation of Wong-Zakai type(see[74])of(2.13)for future work.Note however that(7.23)has already been explored in[12,29,72]in an infinite dimensional fluids context for pathwise solutions and in[73]for martingale solutions to a class of abstract,nonlinear,stochastic PDEs.

    7.3.3 Stochastic forcing of functionals

    Finally,we examine the case when we stochastically force functionals of the unknown,i.e.,terms which have a non-local dependence on the solution U.For example consider,for k≥1 continuous(not necessarily linear)and sufficiently smooth αk=We define

    Here,we interpretin the It? sense.Subject to,for example,

    we obtain aσ from(7.25)which satisfies(2.10).For a“concrete example”of aσ of the form(7.25)which satisfies(7.26),letbe a sequence of elements in L2(M)2withand letαk∈ V satisfying the sumability condition in(7.26).We takeand obtain

    A Appendix:Technical Complements

    We collect here,for the convenience of the reader,various technical results which have been used in the course of the analysis above.While some of the material may be considered to be somewhat “classical”by specialists,we believe that the stochastic type results will be useful to the non-probabilists and that the deterministic results will be helpful for the probabilists.

    A.1 Some convergence properties of measures

    We next briefly review some basic notations of convergence for collections of Borel probability measures.In particular,we highlight a certain abstract convergence lemma that has been used in a crucial way in the passage to the limit several times above.For further details concerning the general theory of convergence in spaces of probability measures,one can refer to,e.g.,[5,65].

    Let(H,ρ)be a completemetric space and denote by Pr(H)the collection of Borel probability measures on H.We recall that a sequenceis said to converge weakly to a measure μ on H(denoted byif and only iffor every bounded continuous functionWe recall that a collectionΛ?Pr(H)is said to be weakly relatively compact if every sequencepossesses a weakly convergent subsequence.On the other hand,we say that Λ ? Pr(H)is tight if,for every?>0 there exists a compact set K?? H such thatμ(K?)≥ 1?? for each μ ∈Λ.The Prokhorov theorem asserts that these two notions,namely tightness and weak compactness of probability measures,are equivalent.

    We also make use of the Skorokhod embedding theorem which states that,wheneveron H,then there exists a probability spaceand a sequence of random variables Xn:such thatand which converges a.s.to a random variablewith

    The following convergence result,found in e.g.[5],relates roughly speaking weak convergence and clustering in probability,and was used to facilitate the proof of(5.26)in Subsection 5.1.3.

    Lemma A.1Let(H,ρ)be an arbitrary metric space.Suppose that Xnand Ynare H-valued random variables,and letbe the associated sequences of the probability laws.If the sequence{μn}n≥0converges weakly to a probability measure μ and if,for all?>0,

    then νnalso converges weakly to μ.

    A.2 An extension of the Doob-Dynkin lemma

    We extend the Doob-Dynkin lemma(see,e.g.,[54])to the case where the image space of the measurable functions are complete separable metric spaces.In order to achieve this goal,let us recall the following notions and results from[21].

    If(?,F)is a measure space and E ? ?,let FE:={B∩E:B ∈F}.Then FEis a sigma algebra of subsets of E,and FEwill be called the relative sigma algebra(of F on E).

    Proposition A.1Let(?,F)be any measurable space and E be any subset of ? (not necessarily in F).Let f be a function on E with values in a Polish space H and measurable with respect to FE.Then f can be extended to a function on all of ?,measurable with respect to F.

    ProofThe proof is direct combining Theorem 4.2.5 and Proposition 4.2.6 in[21].

    Now let(Y,M)be a measure space,X be any set,andψbe a function from X into Y.LetThen ψ?1[M]is a sigma algebra of subsets of X.

    Theorem A.1Given a set X,a measure space(Y,M),and a functionψfrom X into Y,if a function ? on X with values in a Polish space H isψ?1[M]measurable,then there exists an M-measurable function L on Y such that?=L?ψ.

    ProofWhen everψ(u)= ψ(v),we have?(u)= ?(v).Otherwise,let B be a Borel set in H with?(u)∈B but?(v)/∈B.Then??1(B)=ψ?1(C)for some C∈M,withψ(u)∈C but ψ(v)/∈C,a contradiction.Thus,?=L?ψfor some function L from D:=rangeψinto H.For any Borel set E ?H,ψ?1(L?1(E))= ??1(E)=ψ?1(F)for some F ∈ M,so F ∩D=L?1(E)and L is MDmeasurable.By Proposition A.1,L has an M-measurable extension to all of Y.

    A.3 A measurable selection theorem

    We turn now to restate the measurable selection theorem which was proven in[10]and is based on the earlier works(see[11,41]).We employed this result above to establish the existence of adapted solutions to(3.8)in Proposition 3.1.

    Firstly,we recall the definition of a Radon measure.Let X be a locally compact Hausdorff spaces and B(X)be the Borel sigma algebra on X.A Radon measure on X is a measure defined on B(X)that is finite on all compact sets,outer regular on all Borel sets,and inner regular on all open sets(see[26,p.212]).

    Theorem A.2Let X and Y be separable Banach spaces and suppose thatΛ is a“multivalued map”from X into Y,i.e.,a map from X into the subsets of Y.We assume thatΛ takes values in closed,non-empty subsets of Y and that its graph is closed viz.,

    Then,Λ admits a universal Radon measurable section,Γ,that is there exists a mapΓ:X →Y such thatΓx∈Λx for every x,and such thatΓ is Radon measurable for every Radon measure on X.

    Remark A.1Note that since X is a separable Banach space,any probability measure on X is Radon;this is because any separable Banach space is a Polish space(separable and complete metric space)and that every Polish space is a Radon space(a Hausdorff space X is called a Radon space if every finite Borel measure on X is a Radon measure,i.e.,is inner regular(see[66]).

    The following results are from[20,66].The final goal is to establish Corollary A.1 below,which we have employed in the article to prove that the mapχdefined in(3.17)(see Subsection 3.2)is universally Radon measurable.For that purpose,we need to introduce the following results(from Proposition A.2 to Theorem A.3).

    Definition A.1(Lusinμ-Measurable)Let X be a topological space.Letμ be a Radon measure on X and let h map X into Y,where Y is a Hausdorff topological space.Then the mapping h is said to be Lusinμ-measurable if,for every compact set K ?X and everyδ>0,there exists a compact set Kδ?K withμ(K?Kδ)≤δsuch that h restricted to Kδis continuous.

    Proposition A.2A function whose restriction to every compact set is continuous,is Lusin measurable for every Radon measure(see[66,p.25]).

    Proposition A.3The assumptions are the same as in Definition A.1.If h:is Lusin μ-measurable,then h isμ-measurable,and conversely,if Y is metrizable and separable,then everyμ-measurable function is also Lusin μ-measurable(see[66,p.26]).

    Theorem A.3Let X,Y and Z be separable Banach spaces andμbe a Radon measure on X.Letφ:be aμ-measurable mapping.LetΓ:be universally Radon measurable.Then G:=Γ?φ isμ-measurable on X.

    ProofFrom Proposition A.3,φ is Lusinμ-measurable.Then Theorem A.3 follows from the proof of Theorem 3.2 in[10].

    Corollary A.1Let X,Y and Z be separable Banach spaces andbe a continuous mapping.Letbe universally Radon measurable.Then G:=Γ?φis universally Radon measurable.

    ProofThis can be directly deduced from Proposition A.2 and Theorem A.3.

    A.4 Compact embedding results

    In order to establish the compactness of a sequence of probability measures associated with the solutions to(3.3),we made use of the following compact embedding theorem which is close to that found in[69]and of course generalizes the classical Aubin-Lions compactness theorem(see[2]).

    Proposition A.4Let Z??Y?X be a collection of three Banach spaces with Z compactly embedded in Y and Y continuously embedded in X.

    (i)Suppose thatis a bounded subset of Lp(R,Z)∩L∞(R,Y),where 1

    uniformly forand that there exists L>0 such that

    Then,the setis relatively compact in Lp(R,Y).

    (ii)For T>0,if G is a bounded subset of Lp(0,T,Z)∩L∞(0,T,Y)and

    uniformly for elements in G,then G is relatively compact in Lp(0,T,Y).

    ProofThe proof is a fairly straightforward generalization of[70,Theorem 13.2].Observe that if q>p,then(A.2)and(A.3)together imply that

    uniformly for g∈G.Therefore there is no loss of generality in supposing that q≤p in what follows.

    For a>0,define the averaging operator Jaaccording to

    We takeArguing exactly as in[69],we have,for a>0,thatis relatively compact in Lp(R;Y).

    To show thatis itself relatively compact in Lp(R;Y),we prove that it is a totally bounded subset of Lp(R;Y);in other words,we prove that,for every?>0,there exists finitely many elements g1,···,gNin Lp(R,Y)such that G is contained in the union of the ?balls centered at these points.

    Again,arguing exactly as in[69],we have that,as a consequence of(A.2),for everyδ>0 there exists a=a(δ)>0 such that

    On the other hand,from[71,Chapter 3,Lemma 2.1],we infer that,for everyη>0,there exists Cη>0 such that,for every g∈Lp(R,Z),

    The last inequality follows from the fact thatfor all f∈Lp(R,Z).Now,on the other hand,we have

    Fix?>0.Letand letand pick a>0,sufficiently small,so that(A.5)holds forwhere Cηis the constant corresponding toηin(A.6).Using thatis precompact inwe next choose a finite collectionsuch that the-balls centered atcoverNow,with these various choices,we have that for anythere existssuch thatAs such,we employ(A.6)withfollowed by(A.7)and estimate

    Since,?>0 is arbitrary to begin with,this shows that G is a totally bounded subset of Lp(R;Y),and we thus infer(i).The second item(ii)follows directly from(i)as in[69].The proof of Proposition A.4 is therefore complete.

    AcknowledgementsThe authors have benefited from the hospitality of the department of mathematics Virginia Tech and from the Newton institute for mathematical sciences,University of Cambridge where the final stage of the writing was completed.The authors wish to thank Arnaud Debussche for his help with the use of the universally Radon measurable selection theorem.The authors also thank the referee(s)for bringing their attention to the article[3]which they regrettably overlooked.

    [1]Arnold,L.,Stochastic differential equations:Theory and applications,translated from the German,Wiley-Interscience,John Wiley Sons,New York,1974.

    [2]Aubin J.-P.,Approximation of elliptic boundary-value problems,Wiley-Interscience,Pure and Applied Mathematics,Vol.XXVI,A Division of John Wiley Sons,Inc.,New York-London-Sydney,1972.

    [3]Brze?niak,Z.,Carelli,E.and Prohl,A.,Finite-element-based discretizations of the incompressible Navier-Stokes equations with multiplicative random forcing,IMA J.Numer.Anal.,33(3),2013,771–824.

    [4]Bensoussan,A.,Stochastic Navier-Stokes equations,Acta Appl.Math.,38(3),1995,267–304.

    [5]Billingsley,P.,Convergence of probability measures,2nd edition,Wiley Series in Probability and Statistics:Probability and Statistics,John Wiley Sons Inc.,New York,1999.

    [6]Bjerknes,V.,Das problem der wettervorhersage,betrachtet vom standpunkte der mechanik und der physik,Meteorol.Z.,21,1904,1–7.

    [7]Brézis,H.,Problèmes unilatéraux,J.Math.Pures Appl.,51(9),1972,1–168.

    [8]Browder,F.E.,Nonlinear monotone and accretive operators in Banach spaces,Proc.Nat.Acad.Sci.U.S.A.,61,1968,388–393.

    [9]Berner,J.,Shutts,G.J.,Leutbecher,M.and Palmer,T.N.,A spectral stochastic kinetic energy backscatter scheme and its impact on ow-dependent predictability in the ecmwf ensemble prediction system,J.Atmospheric Sci.,66(3),2009,603–626.

    [10]Bensoussan,A.and Temam,R.,équations stochastiques du type Navier-Stokes,J.Functional Analysis,13,1973,195–222.

    [11]Castaing,C.,Sur les multi-applications measurables,Rev.Fran?caise Informat.Recherche Opérationnell,1(1),1967,91–126.

    [12]Chueshov,I.and Millet,A.,Stochastic two-dimensional hydrodynamical systems:Wong-Zakai approximation and support theorem,Stoch.Anal.Appl.,29(4),2011,570–611.

    [13]Cao,C.and Titi,E.,Global well-posedness of the three-dimensional viscous primitive equations of large scale ocean and atmosphere dynamics,Ann.Math.(2),166(1),2007,245–267.

    [14]De Bouard,A.and Debussche,A.,A semi-discrete scheme for the stochastic nonlinear Schr?dinger equation,Numer.Math.,96(4),2004,733–770.

    [15]Debussche,A.,Glatt-Holtz,N.and Temam,R.,Local martingale and pathwise solutions for an abstract uids model,Phys.D,240(14–15),2011,1123–1144.

    [16]Debussche,A.,Glatt-Holtz,N.,Temam,R.and Ziane,M.,Global existence and regularity for the 3D stochastic primitive equations of the ocean and atmosphere with multiplicative white noise,Nonlinearity,25(7),2012,2093–2118.

    [17]Debussche,A.and Printems,J.,Convergence of a semi-discrete scheme for the stochastic Korteweg-de Vries equation,Discrete Contin.Dyn.Syst.Ser.B,6(4),2006,761–781.

    [18]Da Prato,G.and Debussche,A.,Two-dimensional Navier-Stokes equations driven by a space-time white noise,J.Funct.Anal.,196(1),2002,180–210.

    [19]Da Prato,G.and Zabczyk,J.,Stochastic equations in infinite dimensions,Encyclopedia of Mathematics and Its Applications,vol.44,Cambridge University Press,Cambridge,1992.

    [20]Dunford,N.and Schwartz,J.T.,Linear Operators,Part I,Wiley Classics Library,John Wiley Sons Inc.,New York,1988,General theory,with the assistance of William G.Bade and Robert G.Bartle,Reprint of the 1958 original,A Wiley-Interscience Publication.

    [21]Dudley,R.M.,Real analysis and probability,Cambridge Studies in Advanced Mathematics,vol.74,Cambridge University Press,Cambridge,2002,Revised reprint of the 1989 original.

    [22]Durrett,R.,Probability:Theory and examples,4th edition,Cambridge Series in Statistical and Probabilistic Mathematics,Cambridge University Press,Cambridge,2010.

    [23]Ewald,B.and Penland,C.,Numerical generation of stochastic differential equations in climate models,Special Volume on Computational Methods for the Atmosphere and the Oceans,Handbook of Numerical Analysis,vol.14,Elsevier/North-Holland,Amsterdam,2009,279–306.

    [24]Ewald,B.,Petcu,M.and Temam,R.,Stochastic solutions of the two-dimensional primitive equations of the ocean and atmosphere with an additive noise,Anal.Appl.(Singap.),5(2),2007,183–198.

    [25]Flandoli,F.and Gatarek,D.,Martingale and stationary solutions for stochastic Navier-Stokes equations,Probab.Theory Related Fields,102(3),1995,367–391.

    [26]Folland,G.B.,Real analysis,2nd edition,Pure and Applied Mathematics(New York),John Wiley Sons Inc.,New York,1999,Modern Techniques and Their Applications,A Wiley-Interscience Publication.

    [27]Guo,B.and Huang,D.,3D stochastic primitive equations of the large-scale ocean:Global well-posedness and attractors,Comm.Math.Phys.,286(2),2009,697–723.

    [28]Gy?ongy,I.and Millet,A.,On discretization schemes for stochastic evolution equations,Potential Anal.,23(2),2005,99–134.

    [29]Grecksch,W.and Schmalfu?,B.,Approximation of the stochastic Navier-Stokes equation,Mat.Apl.Comput.,15(3),1996,227–239.

    [30]Glatt-Holtz,N.and Temam,R.,Cauchy convergence schemes for some nonlinear partial differential equations,Applicable Analysis,90(1),2011,85–102.

    [31]Glatt-Holtz,N.and Temam,R.,Pathwise solutions of the 2-D stochastic primitive equations,Applied Mathematics and Optimization,63(3),2011,401–433.

    [32]Glatt-Holtz,N.,Temam,R.and Tribbia,J.,Some remarks on the role of stochastic parameterization in the equations of the ocean and atmosphere,in preparation.

    [33]Glatt-Holtz,N.,Temam,R.and C.Wang,Numerical analysis of the stochastic Navier-Stokes equations:Stability and convergence results,in preparation.

    [34]Glatt-Holtz,N.and Vicol,V.C.,Local and global existence of smooth solutions for the stochastic Euler equations with multiplicative noise,Ann.Probab.,42(1),2014,80–145.

    [35]Glatt-Holtz,N.and Ziane,M.,The stochastic primitive equations in two space dimensions with multiplicative noise,Discrete Contin,Dyn.Syst.Ser.B,10(4),2008,801–822.

    [36]Hasselmann,K.,Stochastic climate models,part I:Theory,Tellus,28,1976,474–485.

    [37]Horsthemke,W.and Lefever,R.,Noise-induced transitions:Theory and applications in physics,chemistry and biology,Springer-Verlag,New York,1984.

    [38]Kobelkov,G.M.,Existence of a solution “in the large” for the 3D large-scale ocean dynamics equations,C.R.Math.Acad.Sci.Paris,343(4),2006,283–286.

    [39]Kobelkov,G.M.,Existence of a solution “in the large” for ocean dynamics equations,J.Math.Fluid Mech.,9(4),2007,588–610.

    [40]Kloeden,P.and Platen,E.,Numerical solution of stochastic differential equations,Applications of Mathematics(New York),vol.23,Springer-Verlag,Berlin,1992.

    [41]Kuratowski,K.and Ryll-Nardzewski,C.,A general theorem on selectors,Bull.Acad.Polon.Sci.Sér.Sci.Math.Astronom.Phys.,13,1965,397–403.

    [42]Karatzas,I.and Shreve,S.E.,Brownian motion and stochastic calculus,2nd edition,Graduate Texts in Mathematics,vol.113,Springer-Verlag,New York,1991.

    [43]Kukavica,I.and Ziane,M.,On the regularity of the primitive equations of the ocean,Nonlinearity,20(12),2007,2739–2753.

    [44]Leray,J.and Lions,J.-L.,Quelques résulatats de Vi?ik sur les problèmes elliptiques nonlinéaires par les méthodes de Minty-Browder(in France),Bull.Soc.Math.,93,1965,97–107.

    [45]Leslie,D.C.and Quarini,G.L.,The application of turbulence theory to the formulation of subgrid modelling procedures,Journal of Fluid Mechanics,91,1979,65–91.

    [46]Lions,J.-L.,Temam,R.and Wang,S.H.,New formulations of the primitive equations of atmosphere and applications,Nonlinearity,5(2),1992,237–288.

    [47]Lions,J.-L.,Temam,R.and Wang,S.H.,On the equations of the large-scale ocean,Nonlinearity,5(5),1992,1007–1053.

    [48]Lions,J.-L.,Temam,R.and Wang,S.,Models for the coupled atmosphere and ocean(CAO I,II),Comput.Mech.Adv.,1(1),1993,120.

    [49]Minty,G.J.,Monotone(nonlinear)operators in Hilbert space,Duke Math.J.,29,1962,341–346.

    [50]Manna,U,Menaldi,J.L.and Sritharan,S.S.,Stochastic 2-D Navier-Stokes equation with artificial compressibility,Commun.Stoch.Anal.,1(1),2007,123–139.

    [51]Menaldi,J.L.and Sritharan,S.S.,Stochastic 2-D Navier-Stokes equation,Appl.Math.Optim.,46(1),2002,31–53.

    [52]Mason,P.J.and Thomson,D.J.,Stochastic backscatter in large-eddy simulations of boundary layers,Journal of Fluid Mechanics,242,1992,51–78.

    [53]Marion,M.and Temam,R.,Navier-Stokes equations:theory and approximation,Handbook of numerical analysis,Vol.VI,Handb.Numer.Anal.,VI,North-Holland,Amsterdam,1998,503–688.MR 1665429(2000a:76002)

    [54]?ksendal,B.,Stochastic Differential Equations,An Introduction with Applications,6th edition,Universitext,Springer-Verlag,Berlin,2003.

    [55]Penland,C.and Ewald,B.D.,On modelling physical systems with stochastic models:Diff usion versus Lévy processes,Philos.Trans.R.Soc.Lond.Ser.A Math.Phys.Eng.Sci.,366(1875),2008,2457–2476.

    [56]Pedlosky,J.,Geophysical uid Dynamics,Springer-Verlag,New York,1982.

    [57]Penland,C.,A stochastic approach to nonlinear dynamics:A review,Bulletin of the American Meteorological Society,84,2003,ES43–ES51.

    [58]Prév?t,C.and R?ockner,M.,A concise course on stochastic partial differential equations,Lecture Notes in Mathematics,1905,Springer-Verlag,Berlin,2007.

    [59]Penland,C.and Sardeshmukh,P.D.,The optimal growth of tropical sea surface temperature anomalies,Journal of Climate,8(8),1995,1999–2024.

    [60]Petcu,M.,Temam,R.and Ziane,M.,Some mathematical problems in geophysical fluid dynamics,Special Volume on Computational Methods for the Atmosphere and the Oceans,Handbook of Numerical Analysis,14,Elsevier,2008,577–750.

    [61]Richardson,L.F.,Weather prediction by numerical process,with a foreword by Peter Lynch,2nd edition,Cambridge Mathematical Library,Cambridge University Press,Cambridge,2007.

    [62]Rose,H.A.,Eddy diffusivity,eddy noise and subgrid-scale modelling,Journal of Fluid Mechanics,81,1977,719–734.

    [63]Rozovskii,B.,Temam,R.and Tribbia,J.,AIM Workshop:Mathematical and Geophysical Fluid Dynamics,Analytical and Stochastic Methods,Palo Alto,2006.

    [64]Rousseau,A,Temam,R.M.and Tribbia,J.J.,Boundary value problems for the inviscid primitive equations in limited domains,Handbook of numerical analysis,Vol.XIV,Special volume:Computational methods for the atmosphere and the oceans,Handb.Numer.Anal.,14,Elsevier/North-Holland,Amsterdam,2009,481–575.

    [65]Revuz,D.and Yor,M.,Continuous martingales and Brownian motion,3rd edition,Grundlehren der Mathematischen Wissenschaften[Fundamental Principles of Mathematical Sciences],293,Springer-Verlag,Berlin,1999.

    [66]Schwartz,L,Radon measures on arbitrary topological spaces and cylindrical measures,Published for the Tata Institute of Fundamental Research,Bombay by Oxford University Press,London,1973,Tata Institute of Fundamental Research Studies in Mathematics,No.6.

    [67]Temam,R.,Sur l’approximation des solutions des équations de Navier-Stokes,C.R.Acad.Sci.Paris Sér.A-B,262,1966,A219–A221.

    [68]Temam,R.,Une méthode d’approximation de la solution des équations de Navier-Stokes(in France),Bull.Soc.Math.,96 1968,115–152.

    [69]Temam,R.,Navier-Stokes equations and nonlinear functional analysis,CBMS-NSF Regional Conference Series in Applied Mathematics,vol.41,Society for Industrial and Applied Mathematics(SIAM),Philadelphia,PA,1983.

    [70]Temam,R.,Navier-Stokes equations and nonlinear functional analysis,2nd edition,CBMS-NSF Regional Conference Series in Applied Mathematics,66,Society for Industrial and Applied Mathematics(SIAM),Philadelphia,PA,1995.

    [71]Temam,R.,Navier-Stokes Equations:Theory and Numerical Analysis,Reprint of the 1984 edition,A.M.S.,Providence,RI,2001.

    [72]Twardowska,K.,An approximation theorem of Wong-Zakai type for stochastic Navier-Stokes equations,Rend.Sem.Mat.Univ.Padova,96,1996,15–36.

    [73]Tessitore,G.and Zabczyk,J.,Wong-Zakai approximations of stochastic evolution equations,J.Evol.Equ.,6(4),2006,621–655.

    [74]Wong,E.and Zakai,M.,On the relation between ordinary and stochastic differential equations,Internat.J.Engrg.Sci.,3,1965,213–229.

    [75]Zidikheri,M.J.and Frederiksen,J.S.,Stochastic subgrid-scale modelling for non-equilibrium geophysical ows,Philosophical Transactions of the Royal Society A:Mathematical,Physical and Engineering Sciences,368(1910),2010,145–160.

    蜜臀久久99精品久久宅男| 免费大片18禁| 边亲边吃奶的免费视频| 久久婷婷青草| 亚洲人与动物交配视频| 欧美一区二区亚洲| 欧美日韩在线观看h| 人人妻人人看人人澡| 国产精品熟女久久久久浪| 少妇人妻久久综合中文| 高清视频免费观看一区二区| 久久精品国产a三级三级三级| 国产 精品1| 精品少妇久久久久久888优播| 日韩av不卡免费在线播放| 夜夜爽夜夜爽视频| 精品一区二区三区视频在线| 男女边吃奶边做爰视频| 美女主播在线视频| 美女脱内裤让男人舔精品视频| 欧美日本视频| 夜夜爽夜夜爽视频| 欧美日韩亚洲高清精品| 99久国产av精品国产电影| 国产成人a∨麻豆精品| 成人18禁高潮啪啪吃奶动态图 | 亚洲欧美精品自产自拍| 80岁老熟妇乱子伦牲交| 一级av片app| 黄色视频在线播放观看不卡| 一级二级三级毛片免费看| 久久精品久久久久久噜噜老黄| 免费观看在线日韩| 成人亚洲精品一区在线观看 | www.av在线官网国产| 午夜视频国产福利| 国产伦在线观看视频一区| 国产在线免费精品| 少妇高潮的动态图| 99国产精品免费福利视频| 国产精品99久久99久久久不卡 | 国产亚洲91精品色在线| freevideosex欧美| 亚洲国产日韩一区二区| 欧美变态另类bdsm刘玥| 如何舔出高潮| 成年人午夜在线观看视频| 青春草亚洲视频在线观看| 午夜日本视频在线| 九九在线视频观看精品| 黄色配什么色好看| 欧美97在线视频| 亚洲av不卡在线观看| 99热这里只有是精品50| 大片电影免费在线观看免费| 国产探花极品一区二区| 一级毛片我不卡| 亚洲精品视频女| 尾随美女入室| 美女中出高潮动态图| 亚洲精品第二区| 中国国产av一级| 我的女老师完整版在线观看| 国产 一区精品| 肉色欧美久久久久久久蜜桃| 日日摸夜夜添夜夜添av毛片| 国产在线一区二区三区精| 晚上一个人看的免费电影| 久久久久国产精品人妻一区二区| 欧美zozozo另类| 色哟哟·www| 亚洲国产精品专区欧美| 久久精品国产自在天天线| av网站免费在线观看视频| 免费看光身美女| 免费人成在线观看视频色| 国产爽快片一区二区三区| 国产爽快片一区二区三区| 国产精品久久久久久精品电影小说 | 国产精品无大码| 欧美xxⅹ黑人| 亚洲成色77777| 大香蕉久久网| 精品视频人人做人人爽| 亚洲不卡免费看| 秋霞在线观看毛片| 国产亚洲一区二区精品| 欧美成人一区二区免费高清观看| 亚洲,一卡二卡三卡| 成人漫画全彩无遮挡| 久久人人爽人人爽人人片va| www.色视频.com| 亚洲激情五月婷婷啪啪| 1000部很黄的大片| 国产成人精品久久久久久| 伦理电影大哥的女人| 日韩电影二区| 亚洲国产成人一精品久久久| 免费黄网站久久成人精品| 亚洲精品成人av观看孕妇| 99久久精品国产国产毛片| 久久6这里有精品| 男女国产视频网站| 精品久久国产蜜桃| 成人18禁高潮啪啪吃奶动态图 | 男男h啪啪无遮挡| 亚洲欧洲日产国产| 成人国产av品久久久| 三级国产精品片| 最近手机中文字幕大全| 午夜老司机福利剧场| 99久久精品国产国产毛片| 啦啦啦中文免费视频观看日本| 国产成人精品婷婷| 啦啦啦在线观看免费高清www| 国产欧美另类精品又又久久亚洲欧美| 最近最新中文字幕免费大全7| 有码 亚洲区| 亚洲一区二区三区欧美精品| 在线观看av片永久免费下载| 夜夜看夜夜爽夜夜摸| 欧美激情国产日韩精品一区| 国产精品不卡视频一区二区| 欧美日本视频| 日韩在线高清观看一区二区三区| 国产欧美日韩精品一区二区| 尤物成人国产欧美一区二区三区| 黄色视频在线播放观看不卡| 国产精品久久久久成人av| 亚洲国产精品成人久久小说| 简卡轻食公司| 下体分泌物呈黄色| 欧美xxxx性猛交bbbb| 中文字幕精品免费在线观看视频 | 成人黄色视频免费在线看| 少妇人妻一区二区三区视频| 亚洲真实伦在线观看| 精华霜和精华液先用哪个| freevideosex欧美| 日韩伦理黄色片| 高清日韩中文字幕在线| 成人国产av品久久久| 欧美极品一区二区三区四区| 伊人久久国产一区二区| 久久久久久久国产电影| 中文字幕人妻熟人妻熟丝袜美| 久久毛片免费看一区二区三区| 久久av网站| 国产在线男女| 免费人成在线观看视频色| 欧美变态另类bdsm刘玥| 人人妻人人爽人人添夜夜欢视频 | 亚洲第一区二区三区不卡| 久久久久久久久久人人人人人人| 亚洲成色77777| 亚洲欧美精品自产自拍| 午夜日本视频在线| 日本wwww免费看| 99热网站在线观看| 中文精品一卡2卡3卡4更新| 精品久久国产蜜桃| 校园人妻丝袜中文字幕| 高清欧美精品videossex| 国产美女午夜福利| 美女视频免费永久观看网站| 亚洲精品国产av蜜桃| 热re99久久精品国产66热6| 建设人人有责人人尽责人人享有的 | 国产亚洲午夜精品一区二区久久| 丰满迷人的少妇在线观看| 国产免费视频播放在线视频| 亚洲综合精品二区| 在现免费观看毛片| 国产中年淑女户外野战色| 晚上一个人看的免费电影| 精品一品国产午夜福利视频| 观看免费一级毛片| 免费看不卡的av| 黄色一级大片看看| 精品熟女少妇av免费看| 久久99蜜桃精品久久| 五月伊人婷婷丁香| 一本—道久久a久久精品蜜桃钙片| av免费在线看不卡| 亚洲精品国产色婷婷电影| 久久人人爽av亚洲精品天堂 | 国产成人a区在线观看| 久久这里有精品视频免费| 欧美+日韩+精品| 伊人久久精品亚洲午夜| 亚洲电影在线观看av| 免费人妻精品一区二区三区视频| 少妇丰满av| 少妇的逼好多水| 97在线视频观看| 亚洲色图综合在线观看| 中文字幕精品免费在线观看视频 | 丰满少妇做爰视频| 精品久久久精品久久久| 日韩亚洲欧美综合| 亚洲欧美一区二区三区国产| 在线免费观看不下载黄p国产| a级毛色黄片| av在线老鸭窝| 精品一品国产午夜福利视频| 欧美变态另类bdsm刘玥| 亚洲精华国产精华液的使用体验| 精品少妇黑人巨大在线播放| 国产男女超爽视频在线观看| 成人亚洲精品一区在线观看 | av网站免费在线观看视频| 两个人的视频大全免费| 永久免费av网站大全| 91aial.com中文字幕在线观看| 国产精品偷伦视频观看了| 久久精品国产自在天天线| av国产免费在线观看| 黑人高潮一二区| 久久久国产一区二区| 黄片无遮挡物在线观看| 亚洲欧美成人综合另类久久久| 我的女老师完整版在线观看| 国产国拍精品亚洲av在线观看| 我要看日韩黄色一级片| 国产成人a∨麻豆精品| 精品久久久精品久久久| 干丝袜人妻中文字幕| 乱码一卡2卡4卡精品| 少妇的逼水好多| 日韩国内少妇激情av| 插逼视频在线观看| 国产精品久久久久久久电影| 国产乱人视频| 国产精品秋霞免费鲁丝片| 日本vs欧美在线观看视频 | 国产伦精品一区二区三区视频9| 国国产精品蜜臀av免费| 天堂8中文在线网| 国产精品久久久久久精品电影小说 | 亚洲成人一二三区av| 国产 一区 欧美 日韩| 亚洲最大成人中文| freevideosex欧美| 亚洲av男天堂| 天美传媒精品一区二区| 成年人午夜在线观看视频| 亚洲精品乱码久久久v下载方式| 人人妻人人爽人人添夜夜欢视频 | 精品亚洲成a人片在线观看 | 久久久久国产网址| 22中文网久久字幕| 日韩大片免费观看网站| 校园人妻丝袜中文字幕| 国产黄色视频一区二区在线观看| 99热这里只有是精品50| 国产成人精品福利久久| 精品国产露脸久久av麻豆| 一区二区三区精品91| 国产精品一及| 超碰av人人做人人爽久久| 久久久色成人| 乱码一卡2卡4卡精品| 人妻制服诱惑在线中文字幕| 日韩一本色道免费dvd| 成人国产麻豆网| 超碰av人人做人人爽久久| 欧美精品亚洲一区二区| 国产免费又黄又爽又色| 亚洲成人av在线免费| 国产精品福利在线免费观看| 在线观看三级黄色| 午夜老司机福利剧场| 成人二区视频| 少妇的逼水好多| 亚洲精品aⅴ在线观看| 一级毛片 在线播放| 色视频在线一区二区三区| 人妻系列 视频| h视频一区二区三区| 久久热精品热| 激情五月婷婷亚洲| 久久久久精品性色| 99热这里只有是精品50| 免费av不卡在线播放| 日韩精品有码人妻一区| 啦啦啦中文免费视频观看日本| 在线免费观看不下载黄p国产| 免费少妇av软件| 老司机影院毛片| 美女主播在线视频| 精品少妇久久久久久888优播| 婷婷色av中文字幕| 91狼人影院| 久久99精品国语久久久| 噜噜噜噜噜久久久久久91| 国产淫片久久久久久久久| 欧美一级a爱片免费观看看| 一级毛片黄色毛片免费观看视频| 少妇人妻久久综合中文| 欧美日韩国产mv在线观看视频 | 天天躁夜夜躁狠狠久久av| 我的女老师完整版在线观看| 亚洲综合精品二区| 亚洲第一av免费看| 男女免费视频国产| 欧美精品国产亚洲| 五月天丁香电影| 男人添女人高潮全过程视频| 色网站视频免费| 亚洲欧美成人综合另类久久久| 免费观看性生交大片5| 亚洲av综合色区一区| 国产成人一区二区在线| 中文字幕av成人在线电影| a级毛片免费高清观看在线播放| 日本欧美国产在线视频| 老师上课跳d突然被开到最大视频| 九草在线视频观看| av国产免费在线观看| 青青草视频在线视频观看| 国产 精品1| 联通29元200g的流量卡| 成人免费观看视频高清| 欧美日韩精品成人综合77777| 久久人人爽av亚洲精品天堂 | 亚洲av二区三区四区| 亚洲怡红院男人天堂| 少妇裸体淫交视频免费看高清| 国产中年淑女户外野战色| 人人妻人人看人人澡| 交换朋友夫妻互换小说| 五月玫瑰六月丁香| 热99国产精品久久久久久7| 老女人水多毛片| 美女脱内裤让男人舔精品视频| 久久99热这里只有精品18| av国产久精品久网站免费入址| 精品99又大又爽又粗少妇毛片| .国产精品久久| 成人国产麻豆网| 91精品伊人久久大香线蕉| 亚洲图色成人| 人妻制服诱惑在线中文字幕| 精品久久久久久久久亚洲| 国产av国产精品国产| 高清毛片免费看| 高清午夜精品一区二区三区| 夫妻午夜视频| 亚洲四区av| 又粗又硬又长又爽又黄的视频| 久久久久网色| av专区在线播放| 亚洲精品乱码久久久久久按摩| 青春草亚洲视频在线观看| 18禁动态无遮挡网站| 在线精品无人区一区二区三 | 国产成人免费无遮挡视频| 中文字幕亚洲精品专区| 成年美女黄网站色视频大全免费 | 欧美日韩亚洲高清精品| 看免费成人av毛片| 日韩三级伦理在线观看| 男人和女人高潮做爰伦理| 国产成人a区在线观看| av网站免费在线观看视频| 一级毛片久久久久久久久女| 久久99热6这里只有精品| 久久精品国产亚洲网站| av视频免费观看在线观看| 蜜臀久久99精品久久宅男| 国精品久久久久久国模美| 尤物成人国产欧美一区二区三区| 天堂中文最新版在线下载| 亚洲内射少妇av| 日本黄色片子视频| 蜜桃在线观看..| 只有这里有精品99| 久久 成人 亚洲| 久久精品国产亚洲av天美| 国产av码专区亚洲av| 少妇人妻久久综合中文| 国产淫片久久久久久久久| 小蜜桃在线观看免费完整版高清| 中文欧美无线码| 男男h啪啪无遮挡| 亚洲国产精品国产精品| 亚洲色图av天堂| 一本色道久久久久久精品综合| 热99国产精品久久久久久7| 少妇精品久久久久久久| 亚洲欧美精品自产自拍| 免费久久久久久久精品成人欧美视频 | 国产伦在线观看视频一区| av国产免费在线观看| 亚洲国产最新在线播放| 99久久精品一区二区三区| av免费观看日本| 亚洲成人手机| 丝袜喷水一区| av在线观看视频网站免费| 国产成人免费无遮挡视频| 18+在线观看网站| 十分钟在线观看高清视频www | 美女xxoo啪啪120秒动态图| 男人狂女人下面高潮的视频| 久久国产精品大桥未久av | 国产精品人妻久久久影院| 韩国av在线不卡| h日本视频在线播放| 精品国产乱码久久久久久小说| 最后的刺客免费高清国语| 秋霞伦理黄片| 欧美日韩在线观看h| 国产免费一区二区三区四区乱码| 99久久精品一区二区三区| 男女下面进入的视频免费午夜| 色婷婷久久久亚洲欧美| 99re6热这里在线精品视频| 日韩制服骚丝袜av| 熟女人妻精品中文字幕| 一个人看的www免费观看视频| 2018国产大陆天天弄谢| 中文字幕亚洲精品专区| 国产女主播在线喷水免费视频网站| 搡老乐熟女国产| 国产乱人偷精品视频| 天天躁夜夜躁狠狠久久av| 久久午夜福利片| 亚洲人成网站在线观看播放| 成人国产麻豆网| 乱系列少妇在线播放| 国产精品一区二区在线观看99| 又粗又硬又长又爽又黄的视频| 性色av一级| 日本-黄色视频高清免费观看| 久久久久人妻精品一区果冻| 亚洲精品一区蜜桃| 男人舔奶头视频| 国语对白做爰xxxⅹ性视频网站| 麻豆成人av视频| 国产精品国产三级国产av玫瑰| 少妇人妻精品综合一区二区| 女人久久www免费人成看片| 麻豆国产97在线/欧美| 亚洲成人一二三区av| 成年美女黄网站色视频大全免费 | 亚洲精品一二三| 色婷婷av一区二区三区视频| 乱系列少妇在线播放| 看免费成人av毛片| 18禁裸乳无遮挡动漫免费视频| 国产黄色视频一区二区在线观看| 不卡视频在线观看欧美| 久久久久久久久大av| 建设人人有责人人尽责人人享有的 | 免费少妇av软件| 日本与韩国留学比较| 我要看黄色一级片免费的| 亚洲,欧美,日韩| 午夜激情久久久久久久| 午夜精品国产一区二区电影| 久久久色成人| 老熟女久久久| 男的添女的下面高潮视频| 卡戴珊不雅视频在线播放| a级一级毛片免费在线观看| 亚洲欧洲国产日韩| 亚洲精品成人av观看孕妇| 国产精品久久久久久久电影| 日本av手机在线免费观看| 蜜桃在线观看..| 一本色道久久久久久精品综合| 麻豆精品久久久久久蜜桃| 大话2 男鬼变身卡| 国产免费一区二区三区四区乱码| 国产精品人妻久久久久久| 亚洲一级一片aⅴ在线观看| 亚洲av综合色区一区| 在线观看av片永久免费下载| 欧美xxxx黑人xx丫x性爽| 久久精品国产亚洲av涩爱| 我的女老师完整版在线观看| 如何舔出高潮| 汤姆久久久久久久影院中文字幕| 日韩亚洲欧美综合| 国产在线视频一区二区| 多毛熟女@视频| tube8黄色片| 国产伦精品一区二区三区视频9| 韩国av在线不卡| 日本黄大片高清| 国产成人a∨麻豆精品| 国产伦在线观看视频一区| 啦啦啦在线观看免费高清www| 国产在线一区二区三区精| 国产深夜福利视频在线观看| 天天躁夜夜躁狠狠久久av| 亚洲综合精品二区| 亚洲国产日韩一区二区| 国产精品爽爽va在线观看网站| 国产成人精品一,二区| 少妇丰满av| 国产无遮挡羞羞视频在线观看| 亚洲第一区二区三区不卡| 亚洲精品国产色婷婷电影| 新久久久久国产一级毛片| 国产精品无大码| 亚洲精品日本国产第一区| 国产成人精品福利久久| 黄色怎么调成土黄色| 国产成人午夜福利电影在线观看| 97超视频在线观看视频| 老熟女久久久| 欧美bdsm另类| 99热6这里只有精品| 高清黄色对白视频在线免费看 | 七月丁香在线播放| 久久精品国产亚洲av天美| 成人黄色视频免费在线看| 国产69精品久久久久777片| 日韩一本色道免费dvd| 国产精品熟女久久久久浪| 亚洲第一区二区三区不卡| 91精品伊人久久大香线蕉| 久久久久国产网址| 最近中文字幕高清免费大全6| 久久av网站| 在线观看国产h片| 夜夜爽夜夜爽视频| 久久久久久久久大av| 高清在线视频一区二区三区| 最新中文字幕久久久久| 免费看日本二区| 亚洲欧美日韩无卡精品| 免费在线观看成人毛片| 男的添女的下面高潮视频| 在现免费观看毛片| 国产精品一区二区在线观看99| 日韩成人av中文字幕在线观看| 在线播放无遮挡| 舔av片在线| 午夜免费男女啪啪视频观看| 国产成人精品婷婷| 新久久久久国产一级毛片| 国产精品秋霞免费鲁丝片| 欧美 日韩 精品 国产| 亚洲欧美精品专区久久| 久久精品久久久久久久性| 国产极品天堂在线| 免费在线观看成人毛片| 亚洲激情五月婷婷啪啪| 成年人午夜在线观看视频| 三级国产精品欧美在线观看| 毛片女人毛片| 天堂中文最新版在线下载| 亚洲va在线va天堂va国产| 国产有黄有色有爽视频| 最近手机中文字幕大全| 成年美女黄网站色视频大全免费 | 九九在线视频观看精品| 亚洲婷婷狠狠爱综合网| 久久久久久久久久久免费av| 久久6这里有精品| 国产欧美亚洲国产| 最近中文字幕高清免费大全6| 国产成人一区二区在线| 天美传媒精品一区二区| 99国产精品免费福利视频| 青青草视频在线视频观看| 午夜视频国产福利| 国国产精品蜜臀av免费| 80岁老熟妇乱子伦牲交| 国国产精品蜜臀av免费| 成人午夜精彩视频在线观看| 97在线视频观看| 亚洲无线观看免费| 观看美女的网站| 欧美激情国产日韩精品一区| 超碰av人人做人人爽久久| 国产伦在线观看视频一区| 在线观看美女被高潮喷水网站| 高清视频免费观看一区二区| 久久青草综合色| 一个人看的www免费观看视频| 99久久综合免费| 国产熟女欧美一区二区| 美女cb高潮喷水在线观看| 永久网站在线| 国产美女午夜福利| 久久久午夜欧美精品| 男人狂女人下面高潮的视频| 国产一区二区在线观看日韩| 国产爽快片一区二区三区| 菩萨蛮人人尽说江南好唐韦庄| 新久久久久国产一级毛片| 午夜激情久久久久久久| 日韩一区二区视频免费看| 欧美精品国产亚洲| av专区在线播放| a级毛片免费高清观看在线播放| 国产av一区二区精品久久 | 最近中文字幕高清免费大全6| 国产欧美亚洲国产| 欧美xxxx黑人xx丫x性爽| 精品熟女少妇av免费看| 下体分泌物呈黄色| 国产免费一级a男人的天堂| 水蜜桃什么品种好| 一区二区三区精品91| 欧美 日韩 精品 国产| 日韩不卡一区二区三区视频在线| 日日啪夜夜爽| av免费在线看不卡| 精品久久久噜噜| 国产男女内射视频|