Asymmetric and Moving-Frame Approaches to the 2D and 3D Boussinesq Equations
Boussinesq systems of nonlinear partial differential equations are fundamental equations in geophysical fluid dynamics. In this paper, we use asymmetric ideas and moving frames to solve the two-dimensional Boussinesq equations with partial viscosity …
Authors: Xiaoping Xu
Asymmetric and Mo ving-F rame Approac hes to the 2D and 3D B oussin esq Equations 1 Xiaopi ng Xu Institute of Mathematics, Academ y of Mathematics & System Sciences Chinese Academy of Sciences, Beijing 100 190, P .R. China 2 De dic ate d to 2008 Beijing O l ymp i c Games Abstract Boussinesq systems of nonlinear partial differential equations are fu ndament al equations in geoph ysical fluid dynamics. In this p ap er, we use asymmetric ideas an d mo ving f rames to solv e the t w o-dimensional Boussin esq equations with partial viscosit y terms stud ied by Chae ( A dv. Math. 203 (2006) , 497-513) and the three-dimensional stratified rotating Boussinesq equations studied b y Hsia, Ma and W a ng ( J. Math. Phys. 48 (2007), no. 6, 0656 0). W e obtain new families of explicit exact solutions w ith m ultiple parameter functions. Man y of them are the p erio dic, quasi-p erio d ic, ap erio dic solutions that may ha ve pr actica l significance. By F ourier expansion and some of our solutions, on e can obtain discon tin uous solutions. In add ition, Lie p oint symmetries are used to simp lify our arguments. 1 In tro duction Both the atmospheric and o ceanic flo ws are influenced by the rotat io n of the earth. In fact, the fast rotation and small a sp ect ra tio a r e t w o main characteristic s o f the large scale atmospheric and o ceanic flo ws. The small aspect ratio c haracteristic leads to the primitiv e equations, and the fast rotatio n leads to the quasi-geostropic equations (cf. [2], [6], [7], [9]). A main ob j ective in climate dynamics and in geoph ysical fluid dynamics is to understand and predict the p erio dic, quasi-p erio dic, ap erio dic, and fully turbulent c haracteristics of the lar g e scale atmospheric and o ceanic flows (e.g., cf. [4], [5]). 1 2000 Mathematical Sub ject Classificatio n. Pr imary 35C05, 35Q55 ; Secondar y 37K 10. 2 Research supp orted by China NSF 1 04310 40 1 The Bo ussines q sys tem for the incompressible fluid follows in R 2 is u t + uu x + v u y − ν ∆ u = − p x , v t + uv x + v v y − ν ∆ v − θ = − p y , (1 . 1) θ t + uθ x + v θ y − κ ∆ θ = 0 , u x + v y = 0 , (1 . 2) where ( u, v ) is the v elo city v ector field, p is the scalar pressure, θ is the scalar temp erature, ν ≥ 0 is the viscosit y and κ ≥ 0 is the t hermal diffusivit y . The ab ov e system is a simple mo del in atmospheric sciences (e.g., cf. [8]). Chae [1] prov ed the g lobal regularity , and Hou a nd Li [3] obta ined the w ell-p osedness of the ab o v e system. Aon ther slightly simplified version of the system of primitiv e equations is the three- dimensional stratified rot a ting Boussinesq system (e.g., cf. [7], [9]): u t + uu x + v u y + w u z − 1 R 0 v = σ (∆ u − p x ) , (1 . 3) v t + uv x + v v y + w v z + 1 R 0 u = σ (∆ v − p y ) , (1 . 4) w t + uw x + v w y + w w z − σ R T = σ (∆ w − p z ) , (1 . 5) T t + uT x + v T y + w T z = ∆ T + w , (1 . 6) u x + v y + w z = 0 , (1 . 7) where ( u, v , w ) is the v elo cit y v ector filed, T is the temp erature function, p is the pressure function, σ is the Prandtle n umber, R is the thermal Ra yleigh n um b er and R 0 is the Rossb y n um b er. Moreov er, t he vec tor (1 / R 0 )( − v , u, 0) represen ts the Coriolis force and the term w in (1.6) is deriv ed using s tratificatio n. So the abov e equations are the ex tensions of Navier-Stok es equations by adding the Coriolis f orce and the stratified temp erature equation. Due t o the Corio lis force, the t w o-dimensional system (1 .1 ) and (1.2) is not a sp ecial case of the abov e three-dimens ional syste m. Hsia, Ma and W ang [4] studied the bifurcation and p erio dic solutions of the ab ov e sy stem (1.3)- (1.7). In [1 0], w e used the stable r a nge o f nonlinear term to solv e the equation of nonsta- tionary transonic gas flow. Mor eov er, w e [11] solve d the three-dimensional Na vior-Stokes equations by asymmetric tec hniques and mo ving fra mes. Based on the algebraic charac- teristics of the ab ov e equations, w e use in this pap er asymmetric ideas and mo ving frames to solv e the a b o v e tw o Bo ussinesq systems o f partial differen tial equ ations. Ne w families of explicit exact solutions with m ultiple parameter functions are obta ined. Many of them are the perio dic, quasi-p erio dic, ap erio dic solutions that ma y hav e practical significance. Using F ourier expansion and some of our solutions, o ne can obtain discon tin uous solutions. The symmetry transformatio ns for these equations are used to simplify o ur ar g umen ts. 2 F or con v enience, w e a lwa ys assume that all the in v olv ed partial deriv atives of related functions alw a ys exist and w e can c hange orders of taking partial deriv ativ es. The pa- rameter f unctions are so chosen that the in volv ed expressions mak e sense . W e also use prime ′ to denote the deriv a tiv e of a ny one-v a riable function. Observ e that the tw o- dimensional Boussinesq system (1.1) and (1.2) is in v arian t under the action of the follow ing symmetry t r ansformation: T ( u ) = a − 1 ǫ 1 u ( a 2 ( t + b ) , aǫ 1 ( x + α ) , aǫ 2 ( y + β )) − α ′ , (1 . 8) T ( v ) = a − 1 ǫ 2 v ( a 2 ( t + b ) , a ( x + α ) , a ( y + β )) − β ′ , (1 . 9) T ( p ) = a − 2 p ( a 2 ( t + b ) , aǫ 1 ( x + α ) , aǫ 2 ( y + β )) + α ′ ′ x + β ′ ′ y + γ , (1 . 10) T ( θ ) = a − 3 ǫ 2 θ ( a 2 ( t + b ) , aǫ 1 ( x + α ) , aǫ 2 ( y + β )) , (1 . 11) where a, b ∈ R with a 6 = 0, ǫ 1 , ǫ 2 ∈ { 1 , − 1 } and α , β , γ are arbitrary functions of t . The ab ov e transformat io n transforms a solution of t he equation (1.1) and (1.2) in to another solution with additional three parameter functions. Denote ~ x = ( x, y ). The three-dimensional stratified rotating Boussinesq system is in v ar ia n t under the f o llo wing transformat io ns: T 1 [( u, v , w )] = (( u ( t + b, ~ xA, ǫz ) , v ( t + b, ~ xA ) , ǫz ) A, ǫw ) , (1 . 12) T 1 ( p ) = p ( t + b, ~ xA, ǫz ) , T 1 ( T ) = T ( t + b, ~ xA, ǫz ); (1 . 13) T 2 ( u ) = u ( t, x + α, y + β , z + γ ) − α ′ , T 2 ( v ) = v ( t, x + α , y + β , z + γ ) − β ′ , (1 . 14) T 2 ( w ) = w ( t, x + α, y + β , z + γ ) − γ ′ , T 2 ( T ) = T ( t, x + α , y + β , z + γ ) − γ , (1 . 15) T 2 ( p ) = p ( t, x + α, y + β , z + γ ) + σ − 1 ( α ′ ′ x + β ′ ′ y + γ ′ ′ z ) − Rγ z + µ ; (1 . 16) where ǫ = ± 1, b ∈ R , A ∈ O (2 , R ) , and α , β , γ , µ are arbitrary functions of t . T he abov e transformations transform a solution of the equation (1.3)- (1.7) into a nother solution. In particular, applying the transformatio n T 2 to an y solution in this pa p er yields another solution with extra four parameter functions. T o simplify problems, w e alwa ys solv e the Boussinesq systems mo dulo the ab ov e cor- resp onding symmetry transformatio ns, whic h is an idea that geometers and top ologists often use. The pap er is org anized as follows . In Section 2 , w e solv e the tw o-dimensional Bo ussi- nesq equations (1.1 ) -(1.2) a nd obtain fo ur fa milies of explicit exact solutions. In Section 3, w e presen t a n approach with u , v , w , T linear in x, y to the equations (1.3)-(1 .7 ), and obtain t w o families of explicit exact solutions. Assuming u z = v z = w z z = T z z = 0 in 3 Section 4, w e find another t w o families of explicit exact solutions of the equations (1.3)- (1.7). In Section 5, w e obtain a family of explicit exact solutions of ( 1 .3)-(1.7) that are indep enden t of x . The status can b e c hanged b y applying the transformation in (1.12) and (1 .13) to them. 2 Solutio ns of the 2D B oussin esq Equations In this section, w e solve the t w o-dimensional Boussinesq equations (1.1 ) - (1.2) b y an asym- metric metho d and by an moving frame. According to the second equation in ( 1 .2), w e take the p oten tial form: u = ξ y , v = − ξ x (2 . 1) for some functions ξ in t, x, y . Then the t w o-dimensional Boussinesq equations b ecome ξ y t + ξ y ξ xy − ξ x ξ y y − ν ∆ ξ y = − p x , ξ xt + ξ y ξ xx − ξ x ξ xy − ν ∆ ξ x + θ = p y , (2 . 2) θ t + ξ y θ x − ξ x θ y − κ ∆ θ = 0 . (2 . 3) By our assumption p xy = p y x , the compatible condition of the equations in (2.2) is (∆ ξ ) t + ξ y (∆ ξ ) x − ξ x (∆ ξ ) y − ν ∆ 2 ξ + θ x = 0 . (2 . 4) No w we first solv e the system (2.3) and (2.4). Our a symmetric approach is to a ssume θ = ε ( t, y ) , ξ = φ ( t, y ) + xψ ( t, y ) (2 . 5) for some functions ε, φ a nd ψ in t, y . Then (2.3) b ecomes ε t − ψ ε y − κε y y = 0 . (2 . 6) Moreo v er, (2.4) b ecomes φ y y t + xψ y y t + ( φ y + xψ y ) ψ y y − ψ ( φ y y y + xψ y y y ) − ν ( φ y y y y + xψ y y y y ) = 0 , (2 . 7) equiv alen tly , φ y y t + φ y ψ y y − ψ φ y y y − ν φ y y y y = 0 , (2 . 8) ψ y y t + ψ y ψ y y − ψ ψ y y y − ν ψ y y y y = 0 . (2 . 9) The a b o v e t w o equations are equiv alent to: φ y t + φ y ψ y − ψ φ y y − ν φ y y y = α 1 , (2 . 10) 4 ψ y t + ψ 2 y − ψ ψ y y − ν ψ y y y = α 2 (2 . 11) for some functions α 1 and α 2 of t to b e determined. Let c b e a fixed real constan t and let γ b e a fixed function of t . W e define ζ 1 ( s ) = e γ s − ce − γ s 2 , η 1 = e γ s + ce − γ s 2 , (2 . 12) ζ 0 ( s ) = sin γ s, η 0 ( s ) = cos γ s. (2 . 13) Then η 2 r ( s ) + ( − 1) r ζ 2 r ( s ) = c r (2 . 14) and ∂ s ( ζ r ( s )) = γ η r ( s ) , ∂ s ( η r ( s )) = − ( − 1) r γ ζ r ( s ) , (2 . 15) where we treat 0 0 = 1 when c = r = 0. First we assume ψ = β 1 y + β 2 ζ r ( y ) (2 . 16) for some functions β 1 and β 2 of t , where r = 0 , 1. Then (2.11) b ecomes β ′ 1 + c r β 2 2 γ 2 + β 2 1 + [( β 2 γ ) ′ + ( − 1) r ν β 2 γ 3 + 2 β 1 β 2 γ ] η r ( y ) +( − 1) r β 2 γ ( β 1 γ − γ ′ ) y ζ r ( y ) = α 2 , (2 . 17) whic h is implied by the follow ing equations: β ′ 1 + c r β 2 2 γ 2 + β 2 1 = α 2 , β 1 γ − γ ′ = 0 , (2 . 18) ( β 2 γ ) ′ + ( − 1) r ν β 2 γ 3 + 2 β 1 β 2 γ = 0 . (2 . 19) F or con v enience, we assume γ = √ α ′ for some function α of t . Th us w e ha v e β 1 = γ ′ γ = α ′ ′ 2 α ′ , β 2 = b 1 e − ( − 1) r ν α p ( α ′ ) 3 , b 1 ∈ R . (2 . 20) T o solv e (2.10), w e a ssume φ = β 3 η r ( y ) (2 . 21) for some function β 3 , mo dulo the transformation in (1.8)-(1.1 1 ). Now (2.10) b ecomes [( − 1) r (( β 3 γ ) ′ + β 1 β 3 γ ) + ν β 3 γ 3 ] ζ r ( y ) = − α 1 , (2 . 22) whic h is implied by ( − 1) r (( β 3 γ ) ′ + β 1 β 3 γ ) + ν β 3 γ 3 = 0 . (2 . 23) Th us β 3 = b 2 e − ( − 1) r ν α α ′ , (2 . 24) 5 where b 2 is a real constan t. In order to solv e (2.6), w e assume ε = be γ 1 η r ( y ) , (2 . 25) where b is a real constant and γ 1 is a function of t . Then (2.6) is implied by γ ′ 1 η r ( y ) + ( − 1) r β 2 γ γ 1 ζ 2 r ( y ) + κγ 2 γ 1 (( − 1) r η r ( y ) − γ 1 ζ 2 r ( y )) = 0 , (2 . 26) whic h is implied by γ ′ 1 + ( − 1) r κγ 2 γ 1 = 0 , ( − 1) r β 2 − κγ γ 1 = 0 . (2 . 27) Then the first equation implies γ 1 = b 3 e − ( − 1) r κα (2 . 28) for some constan t b 3 . By the second equations in (2.20) and (2.27) , w e hav e: ( − 1) r b 1 e − ( − 1) r ν α p ( α ′ ) 3 = b 3 κ √ α ′ e − ( − 1) r κα . (2 . 29) F or con v enience, we tak e b 1 = ( − 1) r b 2 0 κb 3 , b 0 ∈ R . (2 . 30) Then (2 .29) is implied by α ′ e ( − 1) r ( ν − κ ) α/ 2 = b 0 . (2 . 31) If ν = κ , then w e hav e α = b 0 t + c 0 . Modulo the transformation in (1.8)-(1.1 1 ), we tak e b 0 = 1 and c 0 = 0, that is, α = t . When ν 6 = κ , we similarly tak e b 0 = 1 and α = 2( − 1) r ν − κ ln[( − 1) r ( ν − κ ) t/ 2 + c 0 ] , c 0 ∈ R . (2 . 32) Supp ose ν = κ . Then γ = 1 and φ = b 2 e − ( − 1) r ν t η r ( y ) , ψ = ( − 1) r b 3 ν e − ( − 1) r ν t ζ r ( y ) . (2 . 33) Moreo v er, θ = b exp( b 3 e − ( − 1) r ν t η r ( y )) , (2 . 34) ξ = b 2 e − ( − 1) r ν t η r ( y ) + ( − 1) r b 3 ν e − ( − 1) r ν t xζ r ( y ) (2 . 35) b y (2 .5). According to (2 .1), u = ξ y = ( − 1) r [ − b 2 e − ( − 1) r ν t ζ r ( y ) + b 3 ν e − ( − 1) r ν t xη r ( y )] , (2 . 36) v = − ξ x = − ( − 1) r b 3 ν e − ( − 1) r ν t ζ r ( y ) . (2 . 37) 6 Note u t + uu x + v u y − ν ∆ u = b 2 3 ν 2 c r e − ( − 1) r 2 ν t x, (2 . 38) v t + uv x + v v y − ν ∆ v − θ = v v y − b exp( b 3 e − ( − 1) r ν t η r ( y )) . (2 . 39) By (1.1) , w e hav e p = b Z exp( b 3 e − ( − 1) r ν t η r ( y )) dy − 1 2 b 2 3 ν 2 e − ( − 1) r 2 ν t ( c r x 2 + ζ 2 r ( y )) (2 . 40) mo dulo the t r ansformation in (1.8)- (1.11). Consider the case ν 6 = κ . Then γ = √ α ′ = 1 p ( − 1) r ( ν − κ ) t/ 2 + c 0 (2 . 41) b y (2 .32). Moreo v er, φ = b 2 [( − 1) r ( ν − κ ) t/ 2 + c 0 ] 2 ν / ( κ − ν )+1 η r ( y ) (2 . 42) b y (2 .21) and (2.24 ) . F urthermore, ψ = ( − 1) r ( κ − ν ) y 4[( − 1) r ( ν − κ ) t/ 2 + c 0 ] + ( − 1) r b 3 κ [( − 1) r ( ν − κ ) t/ 2 + c 0 ] 2 ν / ( κ − ν )+3 / 2 ζ r ( y ) (2 . 43) b y (2 .16), (2.20 ) and (2.30). According to (2.25), (2.28) and ( 2.32), θ = be b 3 [( − 1) r ( ν − κ ) t/ 2+ c 0 ] 2 κ/ ( κ − ν ) η r ( y ) . (2 . 44) Similarly , w e hav e u t + uu x + v u y − ν ∆ u = b 2 3 c r κ 2 [( − 1) r ( ν − κ ) t/ 2 + c 0 ] 4 ν / ( κ − ν )+2 x + 3( ν − κ ) 2 x 16[( − 1) r ( ν − κ ) t/ 2 + c 0 ] 2 , (2 . 45) v t + uv x + v v y − ν ∆ − θ = − ψ t + ψ ψ y + ν ψ y y − θ = − be b 3 [( − 1) r ( ν − κ ) t/ 2+ c 0 ] 2 κ/ ( κ − ν ) η r ( y ) + 3 4 b 3 κ ( κ − ν )[( − 1) r ( ν − κ ) t/ 2 + c 0 ] 2 ν / ( κ − ν )+1 / 2 ζ r ( y ) + 3( ν − κ ) 2 y 16[( − 1) r ( ν − κ ) t/ 2 + c 0 ] 2 + b 2 3 2 κ 2 [( − 1) r ( ν − κ ) t/ 2 + c 0 ] 4 ν / ( κ − ν )+3 ∂ y ζ 2 r ( y ) . (2 . 46) According (1.1 ), w e hav e p = b Z e b 3 [( − 1) r ( ν − κ ) t/ 2+ c 0 ] 2 κ/ ( κ − ν ) η r ( y ) dy − b 2 3 2 c r κ 2 [( − 1) r ( ν − κ ) t/ 2 + c 0 ] 4 ν / ( κ − ν )+2 x 2 − 3( ν − κ ) 2 ( x 2 + y 2 ) 32[( − 1) r ( ν − κ ) t/ 2 + c 0 ] 2 − b 2 3 2 κ 2 [( − 1) r ( ν − κ ) t/ 2 + c 0 ] 4 ν / ( κ − ν )+3 ζ 2 r ( y ) + 3 4 ( − 1) r b 3 κ ( κ − ν )[( − 1) r ( ν − κ ) t/ 2 + c 0 ] 2 ν / ( κ − ν )+1 η r ( y ) (2 . 47) 7 mo dulo the t r ansformation in (1.8)- (1.11). Theorem 2.1 . L et b, b 2 , b 3 , c, c 0 ∈ R and let r = 0 , 1 . If ν = κ , we ha ve the solution (2.34), (2.36 ), (2.37) and (2.40) of the two-dimensional Boussinesq e quations (1.1) -(1.2), wher e ζ r ( y ) an d η r ( y ) ar e define d in (2 .12)-(2.13) with γ = 1 . When ν 6 = κ , we have the fol lowing solutions of the two-dimensional Boussine s q e quations (1.1)-(1.2): u = ( − 1) r ( κ − ν ) x 4[( − 1) r ( ν − κ ) t/ 2 + c 0 ] + ( − 1) r b 3 κ [( − 1) r ( ν − κ ) t/ 2 + c 0 ] 2 ν / ( κ − ν )+1 xη r ( y ) − ( − 1) r b 2 [( − 1) r ( ν − κ ) t/ 2 + c 0 ] 2 ν / ( κ − ν )+1 / 2 ζ r ( y ) , (2 . 48) v = ( − 1) r ( ν − κ ) y 4[( − 1) r ( ν − κ ) t/ 2 + c 0 ] − ( − 1) r b 3 κ [( − 1) r ( ν − κ ) t/ 2 + c 0 ] 2 ν / ( κ − ν )+3 / 2 ζ r ( y ) , (2 . 49) θ is given in (2.44) and p is given in (2.47), w her e ζ r ( y ) a n d η r ( y ) a r e defin e d in (2.1 2)- (2.13) with γ = [( − 1) r ( ν − κ ) t/ 2 + c 0 ] − 1 / 2 . Observ e that ψ = 6 ν y − 1 (2 . 50) is another solution of (2.11). In order t o solve (2.10), we assume φ = ∞ X i =1 γ i y i (2 . 51) mo dulo the transformation in (1.8) - (1.11), where γ i are functions of t to b e determined. No w ( 2 .10) b ecomes − 6 ν γ 1 y − 2 − 18 ν γ 2 y − 1 + ∞ X i =1 [ iγ ′ i − ν ( i + 2)( i + 3)( i + 4) γ i +2 ] y i − 1 = α 1 , (2 . 52) equiv alen tly , γ 1 = γ 2 = 0 , α 1 = − 60 ν γ 3 , (2 . 53) iγ ′ i − ν ( i + 2)( i + 3)( i + 4) γ i +2 = 0 , i > 1 . (2 . 54) Th us γ 2 i +2 = 2 iγ ′ 2 i ν (2 i + 2)(2 i + 3)( 2 i + 4) = 0 , i ≥ 1 , (2 . 55) γ 2 i +3 = (2 i + 1) γ ′ 2 i +1 ν (2 i + 3)(2 i + 4)( 2 i + 5) = 360 γ ( i ) 3 ν i (2 i + 2)(2 i + 5)! , i ≥ 1 . (2 . 56) Hence φ = 36 0 ∞ X i =0 α ( i ) y 2 i +3 ν i (2 i + 3)(2 i + 5)! , (2 . 57) where α is an arbitr ary function of t suc h that the series conv erges, say , a p olynomial in t . 8 T o solve (2.6), w e also assume ε = ∞ X i =0 β i y i , (2 . 58) where β i are functions of t . Then (2.6) b ecomes 6 ν β 1 y − 1 + ∞ X i =0 [ β ′ i + ( i + 2)(6 ν − ( i + 1) κ ) β i +2 ] y i = 0 , (2 . 58) that is, β 1 = 0 a nd β ′ i − ( i + 2)(6 ν + ( i + 1) κ ) β i +2 = 0 , i ≥ 0 . (2 . 59) Hence θ = β + ∞ X i =1 β ( i ) y 2 i 2 i i ! Q i r =1 (6 ν + (2 r − 1) κ ) , (2 . 60) where β is an arbitrary function o f t suc h that the series conv erg es, sa y , a p olynomial in t . In this case, u t + uu x + v u y − ν ∆ u = − 60 ν α , (2 . 61) v t + uv x + v v y − ν ∆ − θ = − 36 ν 2 y − 3 − β − ∞ X i =1 β ( i ) y 2 i 2 i i ! Q i r =1 (6 ν + (2 r − 1) κ ) . (2 . 62) According (1.1 ), w e hav e p = 60 ν αx − 18 ν 2 y − 2 + β y + ∞ X i =1 β ( i ) y 2 i +1 2 i i !(2 i + 1) Q i r =1 (6 ν + (2 r − 1) κ ) (2 . 63) mo dulo the t r ansformation in (1.8)- (1.11). Theorem 2.2 . We have the fol lowing solutions o f the two-dime n sional Boussinesq e q uations (1.1)-(1.2): u = 36 0 ∞ X i =0 α ( i ) y 2 i +2 ν i (2 i + 5)! − 6 ν xy − 2 , v = − 6 ν y − 1 , (2 . 64) θ is given in (2.60) and p is given in (2.63), wher e α and β ar e arbitr ary functions of t such that the r elate d series c onver ge, say, p o l ynom ials in t . Let γ b e a function of t . Denote the mov ing f r a me ˜ = x cos γ + y sin γ , ˆ = y cos γ − x sin γ . (2 . 65) Then ∂ t ( ˜ ) = γ ′ ˆ , ∂ t ( ˆ ) = − γ ′ ˜ . (2 . 66) 9 Moreo v er, ∂ ˜ = cos γ ∂ x + sin γ ∂ y , ∂ ˆ = − sin γ ∂ x + cos γ ∂ y . (2 . 67) In particular, ∆ = ∂ 2 x + ∂ 2 y = ∂ 2 ˜ + ∂ 2 ˆ . (2 . 68) W e assume ξ = φ ( t, ˜ ) − γ ′ 2 ( x 2 + y 2 ) , θ = ψ ( t, ˜ ) , (2 . 69) where φ and ψ are functions in t, ˜ . Then (2 .3 ) b ecomes ψ t − κψ ˜ ˜ = 0 (2 . 70) and (2 .4) b ecomes − 2 γ ′ ′ + φ t ˜ ˜ − ν φ ˜ ˜ ˜ ˜ + ψ ˜ cos γ = 0 . (2 . 71) Mo dulo the tr a nsformation in (1.8)- (1.11), the ab ov e equation is equiv alent to − 2 γ ′ ′ ˜ + φ t ˜ − ν φ ˜ ˜ ˜ + ψ cos γ = 0 . (2 . 72) Assume ν = κ . W e take the following solution of (2 .70): ψ = m X i =1 a i d i e a 2 i κt cos 2 b i + a i ˜ cos b i sin( a 2 i κt sin 2 b i + a i ˜ sin b i + b i + c i ) (2 . 73) where a i , b i , c i , d i are real n umbers. Moreov er, (2.72 ) is equiv alen t to solving the fo llo wing equation: 2 ν γ ′ − γ ′ ′ ˜ 2 + φ t − ν φ ˜ ˜ + [ m X i =1 d i e a 2 i κt cos 2 b i + a i ˜ cos b i × sin ( a 2 i κt sin 2 b i + a i ˜ sin b i + c i )] cos γ = 0 (2 . 74) b y (2 .1). Th us w e hav e the following solution of (2.7 4): φ = − [ m X i =1 d i e a 2 i κt cos 2 b i + a i ˜ cos b i sin( a 2 i κt sin 2 b i + a i ˜ sin b i + c i )] Z cos γ dt + γ ′ ˜ 2 + n X s =1 ˆ d s e ˆ a 2 s κt cos 2 ˆ b s +ˆ a s ˜ cos ˆ b s sin(ˆ a 2 s κt sin 2 ˆ b s + ˆ a s ˜ sin ˆ b s + ˆ c s ) , (2 . 75) where ˆ a s , ˆ b s , ˆ c s , ˆ d s are real n um b ers. Supp ose ν 6 = κ . T o mak e (2.7 2) solv able, we c ho ose the follow ing solution of (2.70): ψ = m X i =1 a i d i e a 2 i κt + a i ˜ . (2 . 76) 10 No w ( 2 .72) is equiv alent to solving the f ollo wing equation: ν γ ′ − γ ′ ′ ˜ 2 + φ t − ν φ ˜ ˜ + m X i =1 d i e a 2 i κt + a i ˜ cos γ = 0 (2 . 77) b y (2 .1). W e obtain the f ollo wing solution of (2.7 7 ): φ = γ ′ ˜ 2 + n X s =1 ˆ d s e ˆ a 2 s κt cos 2 ˆ b s +ˆ a s ˜ cos ˆ b s sin(ˆ a 2 s κt sin 2 ˆ b s + ˆ a s ˜ sin ˆ b s + ˆ c s ) − m X i =1 d i e a 2 i ν t + a i ˜ Z e a 2 i ( κ − ν ) t cos γ dt. (2 . 78) Note u = φ sin γ − γ ′ y , v = γ ′ x − φ cos γ . (2 . 79) By (2.72 ), u t + uu x + v u y − ν ∆ u = ( φ t − ν φ ) sin γ + 2 γ ′ φ cos γ − γ ′ 2 x − γ ′ ′ y = (2 γ ′ ′ ˜ − ψ cos γ ) sin γ + 2 γ ′ φ cos γ − γ ′ 2 x − γ ′ ′ y , = γ ′ ′ ( x sin 2 γ − y cos 2 γ ) + ( 2 γ ′ φ − ψ sin γ ) cos γ − γ ′ 2 x, (2 . 80) v t + uv x + v v y − ν ∆ v − θ = ( ν φ − φ t ) cos γ + 2 γ ′ φ sin γ − γ ′ 2 y + γ ′ ′ x − ψ = ( ψ cos γ − 2 γ ′ ′ ˜ ) cos γ + 2 γ ′ φ sin γ − γ ′ 2 y + γ ′ ′ x − ψ = − γ ′ ′ ( x cos 2 γ + y sin 2 γ ) + (2 γ ′ φ − ψ sin γ ) sin γ − γ ′ 2 y . (2 . 81) According to (1 .1 ), p = γ ′ 2 − γ ′ ′ sin 2 γ 2 x 2 + γ ′ 2 + γ ′ ′ sin 2 γ 2 y 2 + γ ′ ′ xy cos 2 γ + Z ψ d ˜ sin γ − 2 γ ′ φ (2 . 82) mo dulo the t r ansformation in (1.8)- (1.11). Theorem 2.3 . L et γ b e any function of t and denote ˜ = x cos γ + y sin γ . T ake { a i , b i , c i , d i , ˆ a s , ˆ b s , ˆ c s , ˆ d s | i = 1 , ..., m ; s = 1 , ..., n } ⊂ R . (2 . 83) If ν = κ , we have the fol lo wing solutions of the two-d imensional B oussinesq e q uations (1.1)-(1.2): u = − γ ′ y + sin γ { 2 γ ′ ˜ + n X s =1 ˆ a s ˆ d s e ˆ a 2 s κt cos 2 ˆ b s +ˆ a s ˜ cos ˆ b s sin(ˆ a 2 s κt sin 2 ˆ b s + ˆ a s ˜ sin ˆ b s + ˆ b s + ˆ c s ) − [ m X i =1 a i d i e a 2 i κt cos 2 b i + a i ˜ cos b i sin( a 2 i κt sin 2 b i + b i + a i ˜ sin b i + c i )] Z cos γ dt } , (2 . 84) 11 v = γ ′ x − cos γ { 2 γ ′ ˜ + n X s =1 ˆ a s ˆ d s e ˆ a 2 s κt cos 2 ˆ b s +ˆ a s ˜ cos ˆ b s sin(ˆ a 2 s κt sin 2 ˆ b s + ˆ a s ˜ sin ˆ b s + ˆ b s + ˆ c s ) − [ m X i =1 a i d i e a 2 i κt cos 2 b i + a i ˜ cos b i sin( a 2 i κt sin 2 b i + a i ˜ sin b i + b i + c i )] Z cos γ dt } , (2 . 85) θ = ψ in (2.73), and p = (sin γ + 2 γ ′ Z cos γ )[ m X i =1 d i e a 2 i κt cos 2 b i + a i ˜ cos b i sin( a 2 i κt sin 2 b i + a i ˜ sin b i + c i )] + γ ′ 2 − γ ′ ′ sin 2 γ 2 x 2 + γ ′ 2 + γ ′ ′ sin 2 γ 2 y 2 + γ ′ ′ xy cos 2 γ − 2 γ ′ 2 ˜ 2 − 2 γ ′ n X s =1 ˆ d s e ˆ a 2 s κt cos 2 ˆ b s +ˆ a s ˜ cos ˆ b s sin(ˆ a 2 s κt sin 2 ˆ b s + ˆ a s ˜ sin ˆ b s + ˆ c s ) . (2 . 86) When ν 6 = κ , we have the fol lowing so l utions of the two-dimensio n al Bo ussi n esq e qua- tions ( 1 .1)-(1.2): u = { n X s =1 ˆ a s ˆ d s e ˆ a 2 s κt cos 2 ˆ b s +ˆ a s ˜ cos ˆ b s sin(ˆ a 2 s κt sin 2 ˆ b s + ˆ a s ˜ sin ˆ b s + ˆ b s + ˆ c s ) +2 γ ′ ˜ − m X i =1 a i d i e a 2 i ν t + a i ˜ Z e a 2 i ( κ − ν ) t cos γ dt } sin γ − γ ′ y , (2 . 87) v = −{ n X s =1 ˆ a s ˆ d s e ˆ a 2 s κt cos 2 ˆ b s +ˆ a s ˜ cos ˆ b s sin(ˆ a 2 s κt sin 2 ˆ b s + ˆ a s ˜ sin ˆ b s + ˆ b s + ˆ c s ) +2 γ ′ ˜ − m X i =1 a i d i e a 2 i ν t + a i ˜ Z e a 2 i ( κ − ν ) t cos γ dt } cos γ + γ ′ x, (2 . 88) θ = ψ in (2.76), and p = γ ′ 2 − γ ′ ′ sin 2 γ 2 x 2 + γ ′ 2 + γ ′ ′ sin 2 γ 2 y 2 + γ ′ ′ xy cos 2 γ − 2 γ ′ 2 ˜ 2 − 2 γ ′ n X s =1 ˆ d s e ˆ a 2 s κt cos 2 ˆ b s +ˆ a s ˜ cos ˆ b s sin(ˆ a 2 s κt sin 2 ˆ b s + ˆ a s ˜ sin ˆ b s + ˆ c s ) + m X i =1 d i e a 2 i ν t + a i ˜ (2 γ ′ + sin γ ) Z e a 2 i ( κ − ν ) t cos γ dt ) . (2 . 89) Remark 2.4 . By F ourier expansion, w e can use the ab ov e solution to obtain the one dep ending on tw o piecew ise con tin uous f unctions of ˜ . 3 Asymmetric Approac h I to t he 3 D Equati ons Starting from this section, w e use asymmetric approaches dev elop ed in [11] to solv e the stratified rot a ting Boussinesq equations (1.3)- ( 1 .7). 12 F or con v enience o f computation, w e denote Φ 1 = u t + uu x + v u y + w u z − 1 R 0 v − σ ( u xx + u y y + u z z ) , (3 . 1) Φ 2 = v t + uv x + v v y + w v z + 1 R 0 u − σ ( v xx + v y y + v z z ) , (3 . 2) Φ 3 = w t + uw x + v w y + w w z − σ R T − σ ( w xx + w y y + w z z ) . (3 . 3) Then the equations (1.3) - (1.5) b ecome Φ 1 + σ p x = 0 , Φ 2 + σ p y = 0 , Φ 3 + σ p z = 0 . (3 . 4) Our stra t egy is to solve the follo wing compatibilit y conditions: ∂ y (Φ 1 ) = ∂ x (Φ 2 ) , ∂ z (Φ 1 ) = ∂ x (Φ 3 ) , ∂ z (Φ 2 ) = ∂ y (Φ 3 ) . (3 . 5) First we assume u = φ z ( t, z ) x + ς ( t, z ) y + µ ( t, z ) , v = τ ( t, z ) x + ψ z ( t, z ) y + ε ( t, z ) , (3 . 6) w = − φ ( t, z ) − ψ ( t, z ) , T = ϑ ( t, z ) + z , (3 . 7) where φ, ϑ, ς , µ, τ , and ε are f unctions of t, z to b e determined. Then Φ 1 = φ tz x + ς t y + µ t + φ z ( φ z x + ς y + µ ) + ( ς − 1 /R 0 )( τ x + ψ z y + ε ) − ( φ + ψ )( φ z z x + ς z y + µ z ) − σ ( φ z z z x + ς z z y + µ z z ) = [ φ tz + φ 2 z + τ ( ς − 1 /R 0 ) − φ z z ( φ + ψ ) − σ φ z z z ] x +[ ς t + ς φ z + ψ z ( ς − 1 / R 0 ) − ς z ( φ + ψ ) − σ ς z z ] y + µ t + µφ z + ( ς − 1 / R 0 ) ε − µ z ( φ + ψ ) − σ µ z z , (3 . 8) Φ 2 = τ t x + ψ tz y + ε t + ψ z ( τ x + ψ z y + ε ) + ( τ + 1 /R 0 )( φ z x + ς y + µ ) − ( φ + ψ )( τ z x + ψ z z y + ε z ) − σ ( τ z z x + ψ z z z y + ε z z ) = [ ψ tz + ψ 2 z + ς ( τ + 1 /R 0 ) − ( φ + ψ ) ψ z z − σ ψ z z z ] y +[ τ t + τ ψ z + ( τ + 1 / R 0 ) φ z − ( φ + ψ ) τ z − σ τ z z ] x + ε t + εψ z + ( τ + 1 /R 0 ) µ − ( φ + ψ ) ε z − σ ε z z , (3 . 9) Φ 3 = − φ t − ψ t + ( φ + ψ )( φ z + ψ z ) − σ R ( ϑ + z ) + σ ( φ z z + ψ z z ) . (3 . 10) Th us (3.5) is equiv alent to the following system of partial differen tial equations: φ tz + φ 2 z + τ ( ς − 1 /R 0 ) − φ z z ( φ + ψ ) − σ φ z z z = α 1 , (3 . 11) 13 ς t + ς φ z + ψ z ( ς − 1 /R 0 ) − ς z ( φ + ψ ) − σ ς z z = α, (3 . 12) µ t + µφ z + ( ς − 1 /R 0 ) ε − µ z ( φ + ψ ) − σ µ z z = α 2 , (3 . 13) ψ tz + ψ 2 z + ς ( τ + 1 /R 0 ) − ( φ + ψ ) ψ z z − σ ψ z z z = β 1 , (3 . 1 4) τ t + τ ψ z + ( τ + 1 /R 0 ) φ z − ( φ + ψ ) τ z − σ τ z z = α, (3 . 15) ε t + εψ z + ( τ + 1 /R 0 ) µ − ( φ + ψ ) ε z − σ ε z z = β 2 (3 . 16) for some α, α 1 , α 2 , β 1 , β 2 are f unctions of t . Let 0 6 = b and c b e fixed real constan ts. Recall the not io ns in (2.12) a nd (2.13) with γ = b . W e a ssume φ = b − 1 γ 1 ζ r ( z ) , ψ = b − 1 ( γ 2 ζ r ( z ) + γ 3 η r ( z )) , (3 . 17) ς = γ 4 ( γ 2 η r ( z ) − ( − 1) r γ 3 ζ r ( z )) , τ = γ 5 γ 1 η r ( z ) , γ 4 γ 5 = 1 , (3 . 18) where γ i are f unctions of t t o b e determined. Moreov er, (3.11) b ecomes ( γ ′ 1 + ( − 1) r b 2 σ γ 1 − γ 1 γ 5 /R 0 ) η r ( z ) + ( γ 1 + γ 2 ) γ 1 c r = α 1 , (3 . 19) whic h is implied by α 1 = ( γ 1 + γ 2 ) γ 1 c r , (3 . 20) γ ′ 1 + ( − 1) r b 2 σ γ 1 − γ 1 γ 5 /R 0 = 0 . (3 . 21) On the other hand, ( 3 .15) b ecomes [( γ 1 γ 5 ) ′ + γ 1 /R 0 + ( − 1) r b 2 σ γ 1 γ 5 ] η r + γ 1 γ 5 ( γ 1 + γ 2 ) c r = α, (3 . 22) whic h giv es α = γ 1 γ 5 ( γ 1 + γ 2 ) c r , (3 . 23) ( γ 1 γ 5 ) ′ + ( − 1) r b 2 σ γ 1 γ 5 + γ 1 /R 0 = 0 . (3 . 24) Solving (3 .21) and (3.24 ) f or γ 1 and γ 1 γ 5 , w e get γ 1 = b 1 e − ( − 1) r b 2 σt sin t R 0 , γ 1 γ 5 = b 1 e − ( − 1) r b 2 σt cos t R 0 , (3 . 25) where b 1 is a real constan t. In par t icular, we tak e γ 5 = cot t R 0 . (3 . 26) Observ e that (3.12) b ecomes [( γ 2 γ 4 ) ′ + ( − 1) r b 2 σ γ 2 γ 4 − γ 2 /R 0 ] η r ( z ) + γ 4 ( γ 1 γ 2 + γ 2 2 + ( − 1) r γ 2 3 ) c r − ( − 1) r [( γ 3 γ 4 ) ′ + ( − 1) r b 2 σ γ 2 γ 4 − γ 3 /R 0 ] ζ r ( z ) = α (3 . 27) 14 and (3 .14) b ecomes [ γ ′ 2 + ( − 1) r b 2 σ γ 2 + γ 2 γ 4 /R 0 ] η r ( z ) + ( γ 1 γ 2 + γ 2 2 + ( − 1) r γ 2 3 ) c r − ( − 1) r [ γ ′ 3 + ( − 1) r b 2 σ γ 3 + γ 3 γ 4 /R 0 ] ζ r ( z ) = β 1 , (3 . 28) equiv alen tly , α = γ 4 ( γ 1 γ 2 + γ 2 2 + ( − 1) r γ 2 3 ) c r , ( 3 . 29) β 1 = ( γ 1 γ 2 + γ 2 2 + ( − 1) r γ 2 3 ) c r , (3 . 30) ( γ 2 γ 4 ) ′ + ( − 1) r b 2 σ γ 2 γ 4 − γ 2 /R 0 = 0 , (3 . 31) γ ′ 2 + ( − 1) r b 2 σ γ 2 + γ 2 γ 4 /R 0 = 0 , (3 . 32) ( γ 3 γ 4 ) ′ + ( − 1) r b 2 σ γ 2 γ 4 − γ 3 /R 0 = 0 , (3 . 33) γ ′ 3 + ( − 1) r b 2 σ γ 3 + γ 3 γ 4 /R 0 = 0 . (3 . 34) Solving (3 .31)-(3.34) under the assumption γ 4 γ 5 = 1 , we obtain γ 2 γ 4 = b 2 e − ( − 1) r b 2 σt sin t R 0 , γ 2 = b 2 e − ( − 1) r b 2 σt cos t R 0 , (3 . 35) γ 3 γ 4 = b 3 e − ( − 1) r b 2 σt sin t R 0 , γ 3 = b 3 e − ( − 1) r b 2 σt cos t R 0 . (3 . 36) In particular, we ha v e: γ 4 = ta n t R 0 . (3 . 37) According to (3 .2 3) and ( 3.29), γ 1 γ 5 ( γ 1 + γ 2 ) c r = γ 4 ( γ 1 γ 2 + γ 2 2 + ( − 1) r γ 2 3 ) c r , ( 3 . 38) equiv alen tly − 2 b 1 b 2 cos 2 t R 0 + ( b 2 2 − b 2 1 + ( − 1) r b 2 3 ) sin 2 t R 0 = 0 . (3 . 39 ) Th us b 1 b 2 = 0 , b 2 2 − b 2 1 + ( − 1) r b 2 3 = 0 . (3 . 40) So r = 0 , b 2 = 0 , b 1 = b 3 (3 . 41) or r = 1 , b 1 = 0 , b 2 = b 3 . (3 . 42) Assume r = 0 and b 1 6 = 0. Then φ = b − 1 b 1 e − b 2 σt sin bz sin t R 0 , ψ = b − 1 b 1 e − b 2 σt cos bz cos t R 0 , (3 . 43) 15 ς = − b 1 e − b 2 σt sin bz sin t R 0 , τ = b 1 e − b 2 σt cos bz cos t R 0 . (3 . 44) Moreo v er, w e take µ = ε = ϑ = 0. Then Φ 1 = γ 2 1 ( x + γ 5 y ) = b 2 1 e − 2 b 2 σt sin t R 0 x sin t R 0 + y cos t R 0 (3 . 45) b y (3 .8), ( 3 .11)-(3.12 ) , (3.20 ) and (3.23). Similarly Φ 2 = b 2 1 e − 2 b 2 σt cos t R 0 x sin t R 0 + y cos t R 0 . (3 . 46) According to (3 .1 0) Φ 3 = b − 1 R − 1 0 b 1 e − b 2 σt − b − 1 b 2 1 e − 2 b 2 σt cos bz − t R 0 sin bz − t R 0 − Rσ z . (3 . 47) By (3.4) , w e hav e p = Rz 2 2 + b 1 e − b 2 σt b 2 σ R 0 cos bz − t R 0 − b 2 1 e − 2 b 2 σt 2 σ b 2 cos 2 bz − t R 0 − b 2 1 e − 2 b 2 σt 2 σ y 2 cos 2 t R 0 + x 2 sin 2 t R 0 + xy sin 2 t R 0 (3 . 48) mo dulo the t r ansformation in (1.14) - (1.16). Supp ose r = 1 and b 2 6 = 0. Then φ = τ = µ = ε = ϑ = 0 , ψ = b − 1 b 2 e bz + b 2 σt cos t R 0 , ς = b 2 e bz + b 2 σt sin t R 0 . (3 . 4 9) Moreo v er, Φ 1 = Φ 2 = 0 , Φ 3 = b − 1 b 2 R − 1 0 e bz + b 2 σt sin t R 0 + b − 1 b 2 2 e 2( bz + b 2 σt ) cos 2 t R 0 − Rσ z . (3 . 50) According to (3 .4 ), p = Rz 2 2 − b 2 e bz + b 2 σt b 2 σ R 0 sin t R 0 − b 2 2 e 2( bz + b 2 σt ) 2 b 2 σ cos 2 t R 0 (3 . 51) mo dulo the t r ansformation (1.1 4 )-(1.16). Theorem 3.1 . L et b, b 1 , b 2 ∈ R with b 6 = 0 . We have the fol l o wing sol utions of the thr e e-dimension a l str atifie d r otating B oussinesq e quations (1.3 ) -(1.7): (1) u = b 1 e − b 2 σt ( x cos bz − y sin bz ) sin t R 0 , v = b 1 e − b 2 σt ( x cos bz − y sin bz ) cos t R 0 , (3 . 52) w = − b − 1 b 1 e − b 2 σt cos bz − t R 0 , T = z (3 . 53 ) and p is give n in (3.48); (2) u = b 2 e bz + b 2 σt y sin t R 0 , v = b 2 e bz + b 2 σt y cos t R 0 , (3 . 54) 16 w = − b − 1 b 2 e bz + b 2 σt cos t R 0 T = z (3 . 55) and p is give n in (3.51). Next w e assume φ = ς = ψ = τ = 0. Then µ t − 1 R 0 ε − σ µ z z = α 2 , ε t + 1 R 0 ν − σ ε z z = β 2 , ϑ t − ϑ z z = 0 . (3 . 56) Solving them, we get: Theorem 3.2 . L e t a i , b i , c i , d i , ˆ a r , ˆ b r , ˆ c r , ˆ d r , ˜ a s , ˜ b s , ˜ c s , ˜ d s b e r e al numb ers. We have the fol lowing solutions of the thr e e-dim ensional str atifie d r otating Boussinesq e quations (1.3)- (1.7): u = cos t R 0 m X i =1 d i e a 2 i σt cos 2 b i + a i z cos b i sin( a 2 i σ t sin 2 b i + a i z sin b i + c i ) + sin t R 0 n X r =1 ˆ d r e ˆ a 2 r σt cos 2 ˆ b r + a r z cos ˆ b r sin(ˆ a 2 r σ t sin 2 ˆ b r + ˆ a r z sin ˆ b r + ˆ c r ) , (3 . 57) v = − sin t R 0 m X i =1 d i e a 2 i σt cos 2 b i + a i z cos b i sin( a 2 i σ t sin 2 b i + a i z sin b i + c i ) + cos t R 0 n X r =1 ˆ d r e ˆ a 2 r σt cos 2 ˆ b r + a r z cos ˆ b r sin(ˆ a 2 r σ t sin 2 ˆ b r + ˆ a r z sin ˆ b r + ˆ c r ) , (3 . 58) w = 0 , T = z + k X s =1 ˜ a s ˜ d s e ˜ a 2 s t cos 2 ˜ b s +˜ a s z cos ˜ b s sin(˜ a 2 s t sin 2 ˜ b s + ˜ a s z sin ˜ b s + ˜ b s + ˜ c s ) , (3 . 59) p = Rz 2 2 + R m 3 X s =1 ˜ d s e ˜ a 2 s t cos 2 ˜ b s +˜ a s z cos ˜ b s sin(˜ a 2 s t sin 2 ˜ b s + ˜ a s z sin ˜ b s + ˜ c s ) . (3 . 60) Remark 3.3 . By F ourier expansion, w e can use the ab ov e solution to obtain the one dep ending on three ar bitr ary piecewise con tin uous functions of z . 4 Asymmetric Approac h I I to the 3D Equation s In this section, we solv e the stratified rotating Boussinesq equations (1.4)-(1.7 ) under the assumption u z = v z = w z z = T z z = 0 . (4 . 1) Let γ b e a function of t and w e use the mov ing f rame ˜ in (2.65 ). Assume u = f ( t, ˜ ) sin γ − γ ′ y , v = − f ( t, ˜ ) cos γ + γ ′ x, (4 . 2 ) 17 According to (4 .3 ), w e assume w = φ ( t, ) , T = ψ ( t, ) + z , (4 . 3) for some functions f , φ a nd ψ in t and ˜ . Using (2.6 6 )-(2.68), we get Φ 1 = − ( γ ′ 2 + γ ′ /R 0 ) x − γ ′ ′ y + f t sin γ + (2 γ ′ + 1 /R 0 ) f cos γ − σ f ˜ ˜ sin γ , (4 . 4) Φ 2 = − ( γ ′ 2 + γ ′ /R 0 ) y + γ ′ ′ x − f t cos γ + (2 γ ′ + 1 /R 0 ) f sin γ + σ f ˜ ˜ cos γ , (4 . 5) Φ 3 = φ t − σ φ ˜ ˜ − σ R ( ψ + z ) . (4 . 6) By (3.5) , w e hav e − 2 γ ′ ′ + f ˜ t − σ f ˜ ˜ ˜ = 0 , (4 . 7) φ t − σ φ ˜ ˜ − σ Rψ = 0 . (4 . 8) Moreo v er, (1.6) b ecomes ψ t − ψ ˜ ˜ = 0 . (4 . 9) Solving (4 .7), we ha v e: f = 2 γ ′ ˜ + m X i =1 a i d i e a 2 i κt cos 2 b i + a i ˜ cos b i sin( a 2 i κt sin 2 b i + a i ˜ sin b i + b i + c i ) , (4 . 10) where a i , b i , c i , d i are a rbitrary r eal n um b ers. Moreov er, (4.8 ) and (4.9) yield φ = n X r =1 ˆ d r e ˆ a 2 r t cos 2 ˆ b r +ˆ a r ˜ cos ˆ b r sin(ˆ a 2 r t sin 2 ˆ b i + ˆ a r ˜ sin ˆ b r + ˆ c r ) + σ Rtψ , ( 4 . 11) ψ = k X s =1 ˜ d s e ˜ a 2 s t cos 2 ˜ b s +˜ a s ˜ cos ˜ b s sin(˜ a 2 s t sin 2 ˜ b s + ˜ a s ˜ sin ˜ b s + ˜ c s ) (4 . 12) if σ = 1, and φ = n X r =1 ˆ d r e ˆ a 2 r σt cos 2 ˆ b r +ˆ a r ˜ cos ˆ b r sin(ˆ a 2 r σ t sin 2 ˆ b i + ˆ a r ˜ sin ˆ b r + ˆ c r ) + σ R 1 − σ k X s =1 ˜ d s e ˜ a 2 s t cos 2 ˜ b s +˜ a s ˜ cos ˜ b s sin(˜ a 2 s t sin 2 ˜ b s + ˜ a s ˜ sin ˜ b s + ˜ c s ) , (4 . 13) ψ = k X s =1 ˜ a 2 s ˜ d s e ˜ a 2 s t cos 2 ˜ b s +˜ a s ˜ cos ˜ b s sin(˜ a 2 s t sin 2 ˜ b s + ˜ a s ˜ sin ˜ b s + 2 ˜ b s + ˜ c s ) (4 . 14) when σ 6 = 1, where ˆ a r , ˆ b r , ˆ c r , ˆ d r , ˜ a s , ˜ b s , ˜ c s , ˜ d s are a rbitrary real n um b ers. No w Φ 1 = ( γ ′ ′ sin 2 γ − γ ′ 2 − γ ′ /R 0 ) x − γ ′ ′ y cos 2 γ + (2 γ ′ + 1 /R 0 ) f cos γ , (4 . 15) 18 Φ 2 = − ( γ ′ ′ sin 2 γ + γ ′ 2 + γ ′ /R 0 ) y − γ ′ ′ x cos 2 γ + (2 γ ′ + 1 /R 0 ) f sin γ (4 . 16 ) and Φ 3 = − σ Rz . According (3.4 ) , w e hav e p = − 2 γ ′ + 1 /R 0 σ [ γ ′ ˜ 2 + m X i =1 d i e a 2 i κt cos 2 b i + a i ˜ cos b i sin( a 2 i κt sin 2 b i + a i ˜ sin b i + c i )] + R 2 z 2 + ( γ ′ 2 + γ ′ /R 0 )( x 2 + y 2 ) + γ ′ ′ ( y 2 − x 2 ) sin 2 γ 2 σ + γ ′ ′ σ xy cos 2 γ (4 . 17) mo dulo the t r ansformation in (1.14) - (1.16). Theorem 4.1 . L et a i , b i , c i , d i , ˆ a r , ˆ b r , ˆ c r , ˆ d r , ˜ a s , ˜ b s , ˜ c s , ˜ d s b e r e al numb ers and l e t γ b e any function of t . Deno te ˜ = x cos γ + y sin γ . We have the fol lowing solutions of the thr e e-dimension a l str atifie d r otating B oussinesq e quations (1.3 ) -(1.7): u = [ m X i =1 a i d i e a 2 i κt cos 2 b i + a i ˜ cos b i sin( a 2 i κt sin 2 b i + a i ˜ sin b i + b i + c i ) +2 γ ′ ˜ ] sin γ − γ ′ y , (4 . 18) v = [ − m X i =1 a i d i e a 2 i κt cos 2 b i + a i ˜ cos b i sin( a 2 i κt sin 2 b i + a i ˜ sin b i + b i + c i ) +2 γ ′ ˜ ] cos γ + γ ′ x, (4 . 19) p is given in (4.17); w = n X r =1 ˆ d r e ˆ a 2 r t cos 2 ˆ b r +ˆ a r ˜ cos ˆ b r sin(ˆ a 2 r t sin 2 ˆ b i + ˆ a r ˜ sin ˆ b r + ˆ c r ) + σ R t k X s =1 ˜ d s e ˜ a 2 s t cos 2 ˜ b s +˜ a s ˜ cos ˜ b s sin(˜ a 2 s t sin 2 ˜ b s + ˜ a s ˜ sin ˜ b s + ˜ c s ) , (4 . 20) T = z + k X s =1 ˜ d s e ˜ a 2 s t cos 2 ˜ b s +˜ a s ˜ cos ˜ b s sin(˜ a 2 s t sin 2 ˜ b s + ˜ a s ˜ sin ˜ b s + ˜ c s ) (4 . 21) if σ = 1 , a nd w = n X r =1 ˆ d r e ˆ a 2 r σt cos 2 ˆ b r +ˆ a r ˜ cos ˆ b r sin(ˆ a 2 r σ t sin 2 ˆ b i + ˆ a r ˜ sin ˆ b r + ˆ c r ) + σ R 1 − σ k X s =1 ˜ d s e ˜ a 2 s t cos 2 ˜ b s +˜ a s ˜ cos ˜ b s sin(˜ a 2 s t sin 2 ˜ b s + ˜ a s ˜ sin ˜ b s + ˜ c s ) , (4 . 22) T = z + k X s =1 ˜ a 2 s ˜ d s e ˜ a 2 s t cos 2 ˜ b s +˜ a s ˜ cos ˜ b s sin(˜ a 2 s t sin 2 ˜ b s + ˜ a s ˜ sin ˜ b s + 2 ˜ b s + ˜ c s ) (4 . 23) when σ 6 = 1 . 19 Remark 4.2 . By F ourier expansion, w e can use the ab ov e solution to obtain the one dep ending on three ar bitr ary piecewise con tin uous functions of ˜ . Next w e let α b e an y fixed function of t and set = α ( x 2 + y 2 ) . (4 . 24) W e assume u = y φ ( t, ) − α ′ 2 α x, v = − xφ ( t, ) − α ′ 2 α y , (4 . 25) w = ψ ( t, ) + α ′ α z , T = ϑ ( t, ) + z (4 . 26) where φ, ψ and ϑ are functions in t, . Note Φ 1 = − α ′ 2 + 2 αα ′ ′ 4 α 2 x + α ′ 2 R 0 α y + y φ t + x R 0 − α ′ α y φ − xφ 2 − 4 σ αy ( φ ) , (4 . 27) Φ 2 = − α ′ 2 + 2 αα ′ ′ 4 α 2 y − α ′ 2 R 0 α x − xφ t + y R 0 + α ′ α x φ − y φ 2 + 4 σ α x ( φ ) . (4 . 28) According to the first equation in (3 .5), φ t − α ′ α φ − 4 σ α ( φ ) + α ′ 2 R 0 α = 0 , (4 . 29) equiv alen tly , ( φ ) t − α ′ α φ − 4 σ α ( φ ) + α ′ 2 R 0 α = α β ′ (4 . 30) for some function β of t . W rite ˆ φ = φ α + 2 R 0 α − β . (4 . 31) Then (4 .30) b ecomes ˆ φ t − 4 σ α ˆ φ = 0 . (4 . 32) Supp ose ˆ φ = ∞ X i =1 γ i i , (4 . 33) where γ i are f unctions of t t o b e determined. Equation (4.32) yields ( γ i ) t = 4 i ( i + 1 ) σ α γ i +1 . (4 . 34) Hence γ i +1 = ( α − 1 ∂ t ) i ( γ ) i !( i + 1)!(4 σ ) i (4 . 35) for some function γ o f t . Thus ˆ φ = ∞ X i =0 ( α − 1 ∂ t ) i ( γ ) i +1 i !( i + 1)!(4 σ ) i . (4 . 36) 20 By (4.31 ), w e get φ = αβ − 1 2 R 0 + α ∞ X i =0 ( α − 1 ∂ t ) i ( γ ) i i !( i + 1)!(4 σ ) i . (4 . 37) Note Φ 3 = ψ t + α ′ α ψ − 4 σ ( ψ ) − σ R ( ϑ + z ) . (4 . 38 ) By the last t w o equations in (3.5), ψ t + α ′ α ψ − 4 σ ( ψ ) − σ R ϑ = 0 (4 . 39) mo dulo the t r ansformation in (1.14) - (1.16). On the other hand, (1.6) b ecomes ϑ t − 4( ϑ ) = 0 . (4 . 40) Hence ϑ = ∞ X i =0 θ ( i ) 1 i +1 4 i (( i + 1)!) 2 (4 . 41) mo dulo the transformation in (1 .1 4)-(1.16), where θ 1 is an arbitrary function of t . Sub- stituting (4 .41) into (4.39), w e o btain ψ = α − 1 θ 2 + α − 1 ∞ X i =1 θ ( i ) 2 + R P i − 1 r =0 σ i − r ( αθ ( i − s − 1) 1 ) ( s ) (4 σ ) i (( i + 1)!) 2 i +1 , (4 . 42) where θ 2 is another arbitra ry function of t . No w Φ 1 = − α ′ 2 + 2 αα ′ ′ 4 α 2 x + αβ ′ y + x R 0 φ − xφ 2 , (4 . 43) Φ 2 = − α ′ 2 + 2 αα ′ ′ 4 α 2 y − αβ ′ x + y R 0 φ − y φ 2 (4 . 44) b y (4 .27) and (4.28 ) , and Φ 3 = ( α − 1 α ′ − σ R ) z (4 . 45) b y (4 .38). According to (3.4), we obtain p = α ′ 2 + 2 αα ′ ′ 4 σ α 2 + 3 8 σ R 2 0 ( x 2 + y 2 ) + β ′ σ arctan y x + ( R 0 αγ − 1) β σ R 0 ln α ( x 2 + y 2 ) − σ − 1 β 2 2( x 2 + y 2 ) + σ R − α − 1 α ′ R 2 σ z 2 − 1 σ R 0 ∞ X i =0 ( α − 1 ∂ t ) i ( γ ) α i +1 ( x 2 + y 2 ) i +1 (( i + 1)!) 2 (4 σ ) i + α 2 σ ∞ X i,j =0 ( α − 1 ∂ t ) i ( γ )( α − 1 ∂ t ) j ( γ )( α ( x 2 + y 2 )) i + j +1 i ! j !( i + 1)!( j + 1)!( i + j + 1)(4 σ ) i + j + αβ 2 σ ∞ X i =1 ( α − 1 ∂ t ) i ( γ )( α ( x 2 + y 2 )) i i !( i + 1)! i (4 σ ) i (4 . 46) 21 mo dulo the transformation in (1.14 ) - (1.16). By (4.25), (4.26 ), (4.37), (4.4 1 ) and ( 4.42), w e ha v e: Theorem 4.3 L et α, β , γ , θ 1 , θ 2 b e any function of t such that the fol lowing involv e d series c onver ge. We have the fol lowing solutions of the thr e e-dimensional str atifie d r otating Boussinesq e quations (1 .3)-(1.7): u = β y x 2 + y 2 − y 2 R 0 − α ′ 2 α x + αy ∞ X i =0 ( α − 1 ∂ t ) i ( γ ) α i ( x 2 + y 2 ) i i !( i + 1)!(4 σ ) i , (4 . 47) v = x 2 R 0 − α ′ 2 α y − β x x 2 + y 2 + αx ∞ X i =0 ( α − 1 ∂ t ) i ( γ ) α i ( x 2 + y 2 ) i i !( i + 1)!(4 σ ) i , (4 . 48) w = θ 2 ( x 2 + y 2 ) + α ′ α z + 1 α ∞ X i =1 θ ( i ) 2 + R P i − 1 r =0 σ i − r ( αθ ( i − s − 1) 1 ) ( s ) (4 σ ) i (( i + 1)!) 2 α i +1 ( x 2 + y 2 ) i +1 , (4 . 4 9) T = z + ∞ X i =0 θ ( i ) 1 α i +1 ( x 2 + y 2 ) i +1 4 i (( i + 1)!) 2 (4 . 50) and p is give n in (4.46). 5 Asymmetric Approac h I I I to t he 3 D Equati ons In this section, w e solv e (1.3 ) -(1.7) with v x = w x = T x = 0 . Let c b e a real constant. Set = y cos c + z sin c. (5 . 1) Supp ose u = f ( t, ) , v = φ ( t, ) sin c, ( 5 . 2) w = − φ ( t, ) cos c, T = ψ ( t, ) + z , (5 . 3) where f , φ and ψ are functions in t a nd . Then Φ 1 = f t − σ f − sin c R 0 φ, (5 . 4) Φ 2 = ( φ t − σ φ ) sin c + 1 R 0 f , (5 . 5) Φ 3 = ( σ φ − φ t ) cos c − σ R ( ψ + z ) . (5 . 6) By (3.5) , f t − σ f − sin c R 0 φ = 0 , (5 . 7) ( φ t − σ φ ) + sin c R 0 f + σ Rψ cos c = 0 . (5 . 8) 22 Mo dulo (1.14)-( 1 .16), we hav e f t − σ f − sin c R 0 φ = 0 , (5 . 9) φ t − σ φ + sin c R 0 f + σ Rψ cos c = 0 . (5 . 10) Denote ˆ f ˆ φ = cos t si n c R 0 − sin t si n c R 0 sin t sin c R 0 cos t si n c R 0 f φ . (5 . 11) Then (5 .9) and ( 5 .10) b ecome ˆ f t − σ ˆ f − σ Rψ cos c sin t sin c R 0 = 0 , (5 . 12) ˆ φ t − σ ˆ φ + σ Rψ cos c cos t sin c R 0 = 0 . (5 . 13) On the other hand, ( 1 .6) b ecomes ψ t − ψ = 0 . (5 . 14) Assume σ = 1. W e hav e the following solution: ψ = m X i =1 a i d i e a 2 i t cos 2 b i + a i cos b i sin( a 2 i t sin 2 b i + a i sin b i + b i + c i ) , (5 . 15) ˆ f = − RR 0 cot c cos t sin c R 0 m X i =1 a i d i e a 2 i t cos 2 b i + a i cos b i sin( a 2 i t sin 2 b i + a i sin b i + b i + c i ) + n X r =1 ˆ a r ˆ d r e ˆ a 2 r t cos 2 ˆ b r +ˆ a r cos ˆ b r sin(ˆ a 2 r t sin 2 ˆ b i + ˆ a r sin ˆ b r + ˆ b r + ˆ c r ) , (5 . 16 ) ˆ φ = − RR 0 cot c sin t sin c R 0 m X i =1 a i d i e a 2 i t cos 2 b i + a i cos b i sin( a 2 i t sin 2 b i + a i sin b i + b i + c i ) + k X s =1 ˜ a s ˜ d s e ˜ a 2 s t cos 2 ˜ b s +˜ a s cos ˜ b s sin(˜ a 2 s t sin 2 ˜ b s + ˜ a s sin ˜ b s + ˜ b s + ˜ c s ) , (5 . 17) where a i , b i , c i , ˆ a r , ˆ b r , ˆ c r , ˆ d r , ˜ a s , ˜ b s , ˜ c s , ˜ d s are a rbitrary real n um b ers. According to (5.11), f = − RR 0 cot c cos 2 t sin c R 0 m X i =1 a i d i e a 2 i t cos 2 b i + a i cos b i sin( a 2 i t sin 2 b i + a i sin b i + b i + c i ) + cos t sin c R 0 n X r =1 ˆ a r ˆ d r e ˆ a 2 r t cos 2 ˆ b r +ˆ a r cos ˆ b r sin(ˆ a 2 r t sin 2 ˆ b i + ˆ a r sin ˆ b r + ˆ b r + ˆ c r ) + sin t sin c R 0 k X s =1 ˜ a s ˜ d s e ˜ a 2 s t cos 2 ˜ b s +˜ a s cos ˜ b s sin(˜ a 2 s t sin 2 ˜ b s + ˜ a s sin ˜ b s + ˜ b s + ˜ c s ) , (5 . 18) 23 φ = − sin t sin c R 0 n X r =1 ˆ a r ˆ d r e ˆ a 2 r t cos 2 ˆ b r +ˆ a r cos ˆ b r sin(ˆ a 2 r t sin 2 ˆ b i + ˆ a r sin ˆ b r + ˆ b r + ˆ c r ) + cos t sin c R 0 k X s =1 ˜ a s ˜ d s e ˜ a 2 s t cos 2 ˜ b s +˜ a s cos ˜ b s sin(˜ a 2 s t sin 2 ˜ b s + ˜ a s sin ˜ b s + ˜ b s + ˜ c s ) . (5 . 19) Supp ose σ 6 = 1. W e take the f ollo wing solution of (5.1 1 )-(5.14): ψ = m X i =1 a i d i e a 2 i t + a i , (5 . 20) ˆ f = σ R m X i =1 a i d i e a 2 i t + a i cos c h a 2 i (1 − σ ) sin t si n c R 0 − R − 1 0 sin c cos t si n c R 0 i a 4 i (1 − σ ) 2 + R − 2 0 sin 2 c + n X r =1 ˆ a r ˆ d r e ˆ a 2 r σt cos 2 ˆ b r +ˆ a r cos ˆ b r sin(ˆ a 2 r σ t sin 2 ˆ b i + ˆ a r sin ˆ b r + ˆ b r + ˆ c r ) , (5 . 21) ˆ φ = σ R m X i =1 a i d i e a 2 i t + a i cos c h a 2 i ( σ − 1) cos t sin c R 0 − R − 1 0 sin c sin t si n c R 0 i a 4 i (1 − σ ) 2 + R − 2 0 sin 2 c + k X s =1 ˜ a s ˜ d s e ˜ a 2 s σt cos 2 ˜ b s +˜ a s cos ˜ b s sin(˜ a 2 s σ t sin 2 ˜ b s + ˜ a s sin ˜ b s + ˜ b s + ˜ c s ) , (5 . 22) where a i , b i , c i , ˆ a r , ˆ b r , ˆ c r , ˆ d r , ˜ a s , ˜ b s , ˜ c s , ˜ d s are a rbitrary real n um b ers. According to (5.11), f = cos t sin c R 0 n X r =1 ˆ a r ˆ d r e ˆ a 2 r σt cos 2 ˆ b r +ˆ a r cos ˆ b r sin(ˆ a 2 r σ t sin 2 ˆ b i + ˆ a r sin ˆ b r + ˆ b r + ˆ c r ) + sin t sin c R 0 k X s =1 ˜ a s ˜ d s e ˜ a 2 s σt cos 2 ˜ b s +˜ a s cos ˜ b s sin(˜ a 2 s σ t sin 2 ˜ b s + ˜ a s sin ˜ b s + ˜ b s + ˜ c s ) − σ R m X i =1 a i d i e a 2 i t + a i sin 2 c 2 R 0 ( a 4 i (1 − σ ) 2 + R − 2 0 sin 2 c ) , (5 . 23) φ = − sin t sin c R 0 n X r =1 ˆ a r ˆ d r e ˆ a 2 r σt cos 2 ˆ b r +ˆ a r cos ˆ b r sin(ˆ a 2 r σ t sin 2 ˆ b i + ˆ a r sin ˆ b r + ˆ b r + ˆ c r ) + cos t sin c R 0 k X s =1 ˜ a s ˜ d s e ˜ a 2 s σt cos 2 ˜ b s +˜ a s cos ˜ b s sin(˜ a 2 s σ t sin 2 ˜ b s + ˜ a s sin ˜ b s + ˜ b s + ˜ c s ) − σ R m X i =1 a 3 i d i ( σ − 1) e a 2 i t + a i cos c a 4 i (1 − σ ) 2 + R − 2 0 sin 2 c . (5 . 24) By (5.4) -(5.6), ( 5 .9) and (5.10), Φ 1 = 0 , Φ 2 = cos c R 0 f − σ Rψ sin c cos c, (5 . 25) 24 Φ 3 = cos c R 0 f − σ Rψ sin c sin c − σ Rz . (5 . 26) According to (3 .4 ), p = R cos 2 c sin c cos 2 t sin c R 0 m X i =1 d i e a 2 i t cos 2 b i + a i cos b i sin( a 2 i t sin 2 b i + a i sin b i + c i ) − cos c R 0 cos t sin c R 0 n X r =1 ˆ d r e ˆ a 2 r t cos 2 ˆ b r +ˆ a r cos ˆ b r sin(ˆ a 2 r t sin 2 ˆ b i + ˆ a r sin ˆ b r + ˆ c r ) − cos c R 0 sin t sin c R 0 k X s =1 ˜ d s e ˜ a 2 s t cos 2 ˜ b s +˜ a s cos ˜ b s sin(˜ a 2 s t sin 2 ˜ b s + ˜ a s sin ˜ b s + ˜ c s ) + R sin c m X i =1 d i e a 2 i t cos 2 b i + a i cos b i sin( a 2 i t sin 2 b i + a i sin b i + c i ) + R 2 z 2 (5 . 27) mo dulo if σ = 1, and p = − cos c σ R 0 cos t sin c R 0 n X r =1 ˆ d r e ˆ a 2 r σt cos 2 ˆ b r +ˆ a r cos ˆ b r sin(ˆ a 2 r σ t sin 2 ˆ b i + ˆ a r sin ˆ b r + ˆ c r ) − cos c σ R 0 sin t sin c R 0 k X s =1 ˜ d s e ˜ a 2 s σt cos 2 ˜ b s +˜ a s cos ˜ b s sin(˜ a 2 s σ t sin 2 ˜ b s + ˜ a s sin ˜ b s + ˜ c s ) + m X i =1 d i Re a 2 i t + a i sin 2 c cos c 2 R 2 0 ( a 4 i (1 − σ ) 2 + R − 2 0 sin 2 c ) + R sin c m X i =1 d i e a 2 i t + a i + R 2 z 2 , (5 . 28) mo dulo the t r ansformation in (1.14) - (1.16). In summary , w e ha v e: Theorem 5.1 . L et a i , b i , c i , ˆ a r , ˆ b r , ˆ c r , ˆ d r , ˜ a s , ˜ b s , ˜ c s , ˜ d s , c b e arbitr ary r e al numb ers. D e - note = y cos x + z sin c . We have the fol lowing solutions of the thr e e-dimensional str atifie d r otating Boussinesq e quations (1.3)-(1.7): u = f , v = φ sin c, w = − φ cos c, T = ψ + z , (5 . 29) wher e (1) f is given in (5 .18), φ is given i n ( 5 .19), ψ is given in (5 .15) and p is given i n (5.27) if σ = 1 ; (2) f is given in (5.23 ) , φ is given in (5.24), ψ is given in (5.20) and p is g i v en in ( 5 .28) when σ 6 = 1 . Remark 5.2 . By F ourier expansion, w e can use t he ab ov e solution to obtain the one dep ending on three arbitrary pie cewise con tin uous func tions of . Applying the transformation T 1 in (1.12) -(1.13) to the ab ov e solution, w e get a solution in v olving all the v ariables t, x, y , z . 25 References [1] D. 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Ma jda, Intr o duction to PD Es and Waves for the A tmospher e and Oc e a n , Couran t Lecture Note in Mathematics, V ol. 9, AMS and CIMS, 2 0 03. [9] J. P edlosky , Ge oph s ic al F luid D ynamics , 2rd Edition, Springer-v erlag, New Y o rk, 1987. [10] X. Xu, Stable-Range a pproac h to the equation of nonstatio nary tra nsonic gas flows, Quart. Appl. Math. 65 (2007), 52 9-547. [11] X. Xu, Asym metric and mo ving-frame approac hes to Navier-Stok es equations, Quart. Appl. Math. , in press, ar Xiv:0706.1861. 26
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