<?xml version="1.0" encoding="UTF-8"?><!DOCTYPE article  PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd"><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" dtd-version="3.0" xml:lang="en" article-type="research article"><front><journal-meta><journal-id journal-id-type="publisher-id">JAMP</journal-id><journal-title-group><journal-title>Journal of Applied Mathematics and Physics</journal-title></journal-title-group><issn pub-type="epub">2327-4352</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/jamp.2020.89139</article-id><article-id pub-id-type="publisher-id">JAMP-102941</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Physics&amp;Mathematics</subject></subj-group></article-categories><title-group><article-title>
 
 
  Some New Nonlinear Wave Solutions for a Higher-Dimensional Shallow Water Wave Equation
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Longmin</surname><given-names>Dong</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhu</surname><given-names>Guo</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Yinghui</surname><given-names>He</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib></contrib-group><aff id="aff1"><addr-line>Department of Mathematics, Honghe University, Mengzi, China</addr-line></aff><pub-date pub-type="epub"><day>01</day><month>09</month><year>2020</year></pub-date><volume>08</volume><issue>09</issue><fpage>1845</fpage><lpage>1860</lpage><history><date date-type="received"><day>17,</day>	<month>July</month>	<year>2020</year></date><date date-type="rev-recd"><day>15,</day>	<month>September</month>	<year>2020</year>	</date><date date-type="accepted"><day>18,</day>	<month>September</month>	<year>2020</year></date></history><permissions><copyright-statement>&#169; Copyright  2014 by authors and Scientific Research Publishing Inc. </copyright-statement><copyright-year>2014</copyright-year><license><license-p>This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/</license-p></license></permissions><abstract><p>
 
 
  In this manuscript, we first perform a complete Lie symmetry classification for a higher-dimensional shallow water wave equation and then construct the corresponding reduced equations with the obtained Lie symmetries. Moreover, with the extended 
  <em>F</em>-expansion method, we obtain several new nonlinear wave solutions involving differentiable arbitrary functions, expressed by Jacobi elliptic function, Weierstrass elliptic function, hyperbolic function and trigonometric function.
 
</p></abstract><kwd-group><kwd>Shallow Water Wave Equations</kwd><kwd> Nonlinear Wave Solution</kwd><kwd> Lie Symmetry Analysis</kwd><kwd> Extended F-Expansion Method</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>It is well-known that a lot of phenomena in many fields of science can be described by nonlinear evolution equations (NLEEs). Therefore, the investigation of the exact solutions to NLEEs becomes more and more important in mathematical physics. In order to better understand the working to the physical problem, many powerful and direct methods for finding travelling wave solutions of NLEEs have been proposed. However, the study on nonlinear wave solution is few and there is no unified approach. We know that Lie symmetry group [<xref ref-type="bibr" rid="scirp.102941-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.102941-ref2">2</xref>] is efficient to study NLEEs. In decades, Lie symmetry group method has been applied in different fields and several physical models were studied. In this manuscript, a nonlinear wave solution of a higher-dimensional shallow water wave equation is discussed by Lie symmetry analysis combined with extending F-expansion method [<xref ref-type="bibr" rid="scirp.102941-ref3">3</xref>] [<xref ref-type="bibr" rid="scirp.102941-ref4">4</xref>].</p><p>The following higher-dimensional shallow water wave equation is introduced by Wazwaz [<xref ref-type="bibr" rid="scirp.102941-ref5">5</xref>]</p><p>u x z t + u x x x y z − 2 ( u x x u y z + u y u x x z ) − 4 ( u x u x y z + u x y u x z ) = 0. (1)</p><p>We find that Equation (1) can be reduced to the potential KdV equation when z = y = x . The generalized shallow water wave equations studied by Ablowitz [<xref ref-type="bibr" rid="scirp.102941-ref6">6</xref>] arise as reduction of this equation.</p><p>In [<xref ref-type="bibr" rid="scirp.102941-ref5">5</xref>], Wazwaz investigated multiple soliton solutions and multiple singular soliton solutions of Equation (1) and pointed out that this equation is a completely integrable equation. In [<xref ref-type="bibr" rid="scirp.102941-ref7">7</xref>], Yiren Chen and Rui Liu obtained general multiple soliton solutions and some nonlinear wave solutions of Equation (1) by simplified Hirotas method [<xref ref-type="bibr" rid="scirp.102941-ref8">8</xref>] [<xref ref-type="bibr" rid="scirp.102941-ref9">9</xref>] and Dynamical system approach [<xref ref-type="bibr" rid="scirp.102941-ref10">10</xref>]. However, study on nonlinear wave solution is few and Lie symmetry analysis on this equation is not given in related literatures.</p><p>Three goals are set for this work. Firstly, we aim to obtain geometric vector fields of Equation (1). Secondly, we tend to present the symmetry reductions. Finally, we want to get new nonlinear wave solutions of Equation (1) by investigate the reduced equations using extended F-expansion method.</p></sec><sec id="s2"><title>2. Lie Symmetries for Equation (1)</title><p>First of all, let us consider a one-parameter Lie group of infinitesimal transformation:</p><p>x → x + ϵ ξ ( x , y , z , t , u ) , y → y + ϵ η ( x , y , z , t , u ) , z → z + ϵ τ ( x , y , z , t , u ) , t → t + ϵ ξ ( x , y , z , t , u ) , u → u + ϵ ξ ( x , y , z , t , u ) , (2)</p><p>with a small parameter ϵ ≪ 1 . The vector field associated with the above group of transformations can be written as</p><p>V = ξ ( x , y , z , t , u ) ∂ ∂ x + η ( x , y , z , t , u ) ∂ ∂ y + μ ( x , y , z , t , u ) ∂ ∂ z           + τ ( x , y , z , t , u ) ∂ ∂ t + ϕ ( x , y , z , t , u ) ∂ ∂ u . (3)</p><p>The symmetry group of Equation (1) will be generated by the vector field of the form (3). Applying the fourth prolongation p r ( 5 ) V to Equation (1), we find that the coefficient functions ξ , η , μ , τ and ϕ must satisfy the symmetry condition</p><p>ϕ x z t + ϕ x x x y z + 2 ( u y z ϕ x x + u x x ϕ y z + u x x z ϕ y + u y ϕ x x z )   + 4 ( u x y z ϕ x + u x ϕ x y z + u x z ϕ x y + u x y ϕ x z ) = 0 (4)</p><p>where ϕ x , ϕ y , ϕ x x , ϕ x y , ϕ x z , ϕ y z , ϕ x y z , ϕ x x z , ϕ x z t , ϕ x x x y z are the coefficients of p r ( 5 ) V . Furthermore, we have</p><p>ϕ x = D x ( ϕ − ξ u x − η u y − μ u z − τ u t ) + ξ u x x + η u x y + μ u x z + τ u x t , ϕ y = D y ( ϕ − ξ u x − η u y − μ u z − τ u t ) + ξ u x y + η u y y + μ u y z + τ u y t , ϕ x x = D x D x ( ϕ − ξ u x − η u y − μ u z − τ u t ) + ξ u x x x + η u x x y + μ u x x z + τ u x x t , ϕ x y = D y D x ( ϕ − ξ u x − η u y − μ u z − τ u t ) + ξ u x x y + η u x y y + μ u x y z + τ u x y t , ϕ x z = D z D x ( ϕ − ξ u x − η u y − μ u z − τ u t ) + ξ u x x z + η u x y z + μ u x z z + τ u x z t ,</p><p>ϕ y z = D z D y ( ϕ − ξ u x − η u y − μ u z − τ u t ) + ξ u x y z + η u y y z + μ u y z z + τ u y z t , ϕ x y z = D z D y D x ( ϕ − ξ u x − η u y − μ u z − τ u t ) + ξ u x x y z + η u x y y z + μ u x y z z + τ u x y z t , ϕ x x z = D z D D x 2 ( ϕ − ξ u x − η u y − μ u z − τ u t ) + ξ u x x x z + η u x x y z + μ u x x z z + τ u x x z t , ϕ x z t = D t D z D x ( ϕ − ξ u x − η u y − μ u z − τ u t ) + ξ u x x z t + η u x y z t + μ u x z z t + τ u x z t t , ϕ x x x y z = D z D y D x 3 ( ϕ − ξ u x − η u y − μ u z − τ u t ) + ξ   u x x x x y z + η   u x x x y y z + μ   u x x x y z z                     + τ   u x x x y z t , (5)</p><p>where D x 3 = D x D x D x , D x 2 = D x D x , D x , D y , D z and D t are the total derivatives with respect to x , y , z and t respectively.</p><p>Substituting (5) into (4), combined with Equation (1), we can find the determining equations for the symmetry group of Equation (1), then standard symmetry group calculations lead to the following forms of the coefficient functions:</p><p>ξ = 1 4   ( F ′ 1 ( t ) − 2 c 1 ) x + F 5 ( t ) ,   η = ( 1 2 F ′ 1 ( t ) + c 1 ) y + F 3 ( t ) , μ = F 4 ( z ) ,   τ = F 1 ( t ) , ϕ = ( − 1 4 F ′ 1 ( t ) + c 1 2 ) u − 1 8 ( F ″ 1 ( t ) y + 2 F ′ 3 ( t ) ) x − y 2 F ′ 5 ( t ) + F 2 ( z , t ) . (6)</p><p>where F 1 ( t ) , F 2 ( t ) , F 3 ( z , t ) , F 4 ( z ) and F 5 ( t ) are arbitrary functions on their variables, c 1 is an arbitrary constants.</p><p>Thus, according to the Lie symmetry analysis method, the geometric vector fields of Equation (1) can be obtained as follows</p><p>V 1 ( F 1 ) = x 4 F ′ 1 ( t ) ∂ ∂ x + y 2 F ′ 1 ( t ) ∂ ∂ y + F 1 ( t ) ∂ ∂ t − ( u 4 F ′ 1 ( t ) + x y 8 F ″ 1 ( t ) ) ∂ ∂ u , V 2 ( F 2 ) = F 2 ( z , t ) ∂ ∂ u ,   V 3 ( F 3 ) = F 3 ( t ) ∂ ∂ y − x 4 F ′ 3 ( t ) ∂ ∂ u ,   V 4 ( F 4 ) = F 4 ( z ) ∂ ∂ z , V 5 ( F 5 ) = F 5 ( t ) ∂ ∂ x − y 2 F ′ 5 ( t ) ∂ ∂ u ,   V 6 = − x 2 ∂ ∂ x + y   ∂ ∂ y + u ∂ ∂ u , (7)</p><p>the symmetry of Equation (3) can be written as</p><p>V = V 1 ( F 1 ) + V 2 ( F 2 ) + V 3 ( F 3 ) + V 4 ( F 4 ) + V 5 ( F 5 ) + V 6 . (8)</p></sec><sec id="s3"><title>3. Symmetry Reductions</title><p>In terms of the infinitesimals (5), the similarity variables can be obtained by solving the corresponding characteristic equations</p><p>d x ξ = d y η = d z μ = d t τ = d u ϕ , (9)</p><p>or the invariant surface conditions</p><p>Φ = ξ ∂ ∂ x u ( x , y , z , t ) + η ∂ ∂ y u ( x , y , z , t ) + μ ∂ ∂ z u ( x , y , z , t )     + τ ∂ ∂ t u ( x , y , z , t ) − ϕ . (10)</p><p>While solving the above invariant surface conditions, one has to distinguish between cases in which some of the functions F 1 ( t ) , F 2 ( z , t ) , F 3 ( t ) , F 4 ( z ) , F 5 ( t ) and c 1 are identical to zero and cases where they are not. This leads to different relations between the similarity variables ( X , Y , Z , U ) and the original variables ( x , y , z , t , u ) . As a result, we obtain the following cases:</p><p>Case 1. Let c 1 = 1 , F 1 ( t ) = F 2 ( z , t ) = F 3 ( t ) = F 4 ( z ) = F 5 ( t ) = 0 , then</p><p>Φ = − x 2 u x + y   u y − u 2 . (11)</p><p>Solving the differential equation Φ = 0 one can get</p><p>u = U ( Y , z , t ) x ,   Y = x 2 y . (12)</p><p>Substituting (12) into Equation (1), we can reduce it to</p><p>U t z + ( 8 U U Y Y z − 8 U Y U Y z + 9 U Y Y U z + 2 U Y Y z ) Y + ( − 24 U Y Y z U Y − 24 U Y Y U Y z + 24 U Y Y Y z ) Y 2 + 8 U Y Y Y z Y 3 = 0. (13)</p><p>Case 2. Let c 1 = F 1 ( t ) = 1 , F 4 ( z ) = F 5 ( t ) = 0 , then</p><p>Φ = u t − F 2 ( z , t ) + F 3 ( t ) u y + x 4 F ′ 3 ( t ) . (14)</p><p>Solving the differential equation Φ = 0 one can get</p><p>u = U ( x , Y , z ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) ,   Y = y − ∫ F 3 ( t ) d t . (15)</p><p>Substituting (15) into Equation (1), we can reduce it to</p><p>U x x x Y z − 2 ( U x x U Y z + U Y U x x z ) − 4 ( U Y x U x z + U x U x Y z ) = 0. (16)</p><p>Case 3. Let c 1 = 0 , F 1 ( t ) = F 2 ( z , t ) = F 3 ( t ) = 1 , F 5 ( t ) = 0 , then</p><p>Φ = u t + u y + F 4 ( z ) u z − 1. (17)</p><p>Solving the differential equation Φ = 0 one can get</p><p>u = U ( x , Y , Z ) + ∫ 1 F 4 ( z ) d z ,   Y = y − ∫ 1 F 4 ( z ) d z ,   Z = t − ∫ 1 F 4 ( z ) d z . (18)</p><p>Substituting (18) into Equation (1), we can reduce it to</p><p>U x Y Z − U x x x Z Z − U x x x Y Z + 2 U x x ( U Z Z + U Y Z ) + 2 U x x Z ( U z + U y )   + 4 U x ( U x Z Z + U x Y Z ) + 4 U x z ( U x Z + U x Y ) = 0. (19)</p><p>Case 4. Let c 1 = F 1 ( t ) = F 2 ( z , t ) = F 4 ( z , t ) = 0 , F 5 ( t ) = 1 , then</p><p>Φ = u x + F 3 ( t ) u y + x 4 F ′ 3 ( t ) . (20)</p><p>Solving the differential equation Φ = 0 one can get</p><p>u = U ( z , t , Y ) − x 2 8 F ′ 3 ( t ) ,   Y = y − x F 3 ( t ) . (21)</p><p>Substituting (21) into Equation (1), we can reduce it to</p><p>− F 3 ( t ) 3 U Y Y Y Y z − 6 F 3 ( t ) 2 ( U Y U Y Y z + U Y Z U Y Y ) − F 3 ( t ) U t Y z − 1 2 F ′ 3 ( t ) U Y z = 0. (22)</p><p>Case 5. Let c 1 = F 1 ( t ) = F 3 ( t ) = 0 , F 5 ( t ) = 1 , then</p><p>Φ = F 4 ( z ) u z − F 2 ( z , t ) . (23)</p><p>Solving the differential equation Φ = 0 one can get</p><p>u = U ( x , y , t ) + ∫ F 2 ( z , t ) F 4 ( z ) d z . (24)</p><p>Substituting (24) into Equation (1), we find that U ( x , y , t ) is an arbitrary function. That is, the solution of Equation (1) can be expressed as (24).</p><p>Case 6. Let c 1 = F 1 ( t ) = 0 , F 2 ( z , t ) = F 3 ( t ) = 1 , F 4 ( z ) = F 5 ( t ) = 0 , then</p><p>Φ = u y − 1. (25)</p><p>Solving the differential equation Φ = 0 one can get</p><p>u = U ( x , z , t ) + y . (26)</p><p>Substituting (26) into Equation (1), we can reduce it to</p><p>U x t z − 2 U x x z = 0 , (27)</p><p>whose solution is</p><p>U ( x , z , t ) = r 1 ( t , z ) + r 3 ( t , x ) + r 4 ( z , 2 t + x ) , (28)</p><p>where r 1 ( t , z ) , r 3 ( t , x ) and r 4 ( z ,2 t + x ) are arbitrary functions. So, Equation (1) owns the following solution</p><p>u ( x , y , z , t ) = y + r 1 ( t , z ) + r 3 ( t , x ) + r 4 ( z , 2 t + x ) , (29)</p></sec><sec id="s4"><title>4. The New Nonlinear Wave Solutions</title><p>Obviously, it is easier for us to seek the explicit solutions to the reduction equations than to solve Equation (1). For example, we will consider the exact solutions of Equation (16) and Equation (19) by using the extended F-expansion method in this section.</p><sec id="s4_1"><title>4.1. Solutions of Equation (16)</title><p>Using a traveling wave variable of Equation (16) as</p><p>U ( x , Y , t ) = f ( ξ ) ,   ξ = k x + b Y + c z . (30)</p><p>where Y = y − ∫ F 3 ( t ) d t , k , b and c are constants, Equation (16) can be reduced to the following ODE</p><p>k f ( 5 ) − 6 ( f ″ ) 2 − 6 f ′ f ‴ = 0, (31)</p><p>where f ′ = d f d ξ , f ″ = d 2 f d ξ 2 , ⋯ . If let f ′ ( ξ ) = ϕ ( ξ ) , then (31) becomes</p><p>k ϕ ( 4 ) − 6 ( ϕ ′ ) 2 − 6 ϕ ϕ ″ = 0, (32)</p><p>Balancing ϕ ( 4 ) and ϕ ′ 2 in (32), we obtain n + 4 = 2 ( n + 1 ) which gives n = 2 . Suppose that Equation (32) owns the solutions in the form</p><p>ϕ ( ξ ) = A 0 + A 1 F ( ξ ) + A 2 F 2 ( ξ ) + B 1 F ( ξ ) + B 2 F ( ξ ) 2 , (33)</p><p>where F ( ξ ) satisfies the following equation</p><p>( F ′ ( ξ ) ) 2 = h 0 + h 2 F 2 ( ξ ) + h 4 F 4 ( ξ ) , (34)</p><p>where h 0 , h 2 and h 4 are constant.</p><p>Substituting (33) and (34) into Equation (32) and then setting all the coefficients of F k ( k = − 6 , ⋯ , 6 ) of the resulting system to zero, we can obtain the following results.</p><p>A 0 = 2 3   k h 2 , A 1 = 0 , A 2 = 0 , B 1 = 0 , B 2 = 2   k h 0 , (35)</p><p>A 0 = 2 3   k h 2 , A 1 = 0 , A 2 = 2   k h 4 , B 1 = 0 , B 2 = 0 , (36)</p><p>A 0 = 2 3   k h 2 , A 1 = 0 , A 2 = 2   k h 4 , B 1 = 0 , B 2 = 2   k h 0 , (37)</p><p>where h 0 , h 2 and h 4 are arbitrary constants, k is a nonzero constant.</p><p>Substituting (35)-(37) into (33), we obtain respectively the following solutions of Equation (32)</p><p>ϕ ( ξ ) = 2 3 k h 2 + 2 k h 0 F ( ξ ) 2 , (38)</p><p>ϕ ( ξ ) = 2 3 k h 2 + 2 k h 4 F ( ξ ) 2 , (39)</p><p>ϕ ( ξ ) = 2 3 k h 2 + 2 k h 0 F 2 ( ξ ) + 2   k h 4 F ( ξ ) 2 , (40)</p><p>where ξ = k x + b Y + c z = k x + b ( y − ∫ F 3 ( t ) d t ) + c t .</p><p>The solutions of Equation (34) are given in <xref ref-type="table" rid="table1">Table 1</xref>. Combining (38)-(40) with <xref ref-type="table" rid="table1">Table 1</xref>, many exact solutions of Equation (1) can be obtained. For simplicity, we just give out the first case in <xref ref-type="table" rid="table1">Table 1</xref>; the other cases can be discussed similarly.</p><p>When h 0 = 1 , h 2 = −   ( m 2 + 1 ) , h 4 = m 2 , the solution of Equation (33) is F ( ξ ) = sn ( ξ , m ) or F ( ξ ) = cd ( ξ , m ) . Substituting them into Equation (38)-(40), we can obtain the following Jacobi Elliptic function solutions of Equation (32).</p><p>From (38), one has</p><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> Solutions of F ( ξ ) in F ′ 2 = h 0 + h 2 F 2 + h 4 F 4 </title></caption><table><tbody><thead><tr><th align="center" valign="middle" >case</th><th align="center" valign="middle" >h 0</th><th align="center" valign="middle" >h 2</th><th align="center" valign="middle" >h 4</th><th align="center" valign="middle" >F ( ξ )</th></tr></thead><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >− ( m 2 + 1 )</td><td align="center" valign="middle" >m 2</td><td align="center" valign="middle" >sn ( ξ ) , cd ( ξ )</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >1 − m 2</td><td align="center" valign="middle" >m 2 − 1</td><td align="center" valign="middle" >− m 2</td><td align="center" valign="middle" >cn ( ξ )</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >m 2 − 1</td><td align="center" valign="middle" >2 − m 2</td><td align="center" valign="middle" >−1</td><td align="center" valign="middle" >dn ( ξ )</td></tr><tr><td align="center" valign="middle" >4</td><td align="center" valign="middle" >m 2</td><td align="center" valign="middle" >− ( m 2 + 1 )</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >ns ( ξ ) , dc ( ξ )</td></tr><tr><td align="center" valign="middle" >5</td><td align="center" valign="middle" >− m 2</td><td align="center" valign="middle" >2 m 2 − 1</td><td align="center" valign="middle" >1 − m 2</td><td align="center" valign="middle" >nc ( ξ )</td></tr><tr><td align="center" valign="middle" >6</td><td align="center" valign="middle" >−1</td><td align="center" valign="middle" >2 − m 2</td><td align="center" valign="middle" >m 2 − 1</td><td align="center" valign="middle" >nd ( ξ )</td></tr><tr><td align="center" valign="middle" >7</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >2 − m 2</td><td align="center" valign="middle" >1 − m 2</td><td align="center" valign="middle" >sc ( ξ )</td></tr><tr><td align="center" valign="middle" >8</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >2 m 2 − 1</td><td align="center" valign="middle" >− m 2 ( 1 − m 2 )</td><td align="center" valign="middle" >sd ( ξ )</td></tr><tr><td align="center" valign="middle" >9</td><td align="center" valign="middle" >1 − m 2</td><td align="center" valign="middle" >2 − m 2</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >cs ( ξ )</td></tr><tr><td align="center" valign="middle" >10</td><td align="center" valign="middle" >− m 2 ( 1 − m 2 )</td><td align="center" valign="middle" >2 m 2 − 1</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >sd ( ξ )</td></tr><tr><td align="center" valign="middle" >11</td><td align="center" valign="middle" >1 4</td><td align="center" valign="middle" >1 − 2 m 2 2</td><td align="center" valign="middle" >1 4</td><td align="center" valign="middle" >ns ( ξ ) &#177; cs ( ξ )</td></tr><tr><td align="center" valign="middle" >12</td><td align="center" valign="middle" >1 − m 2 4</td><td align="center" valign="middle" >1 + m 2 2</td><td align="center" valign="middle" >1 − m 2 4</td><td align="center" valign="middle" >nc ( ξ ) &#177; sc ( ξ )</td></tr><tr><td align="center" valign="middle" >13</td><td align="center" valign="middle" >m 2 4</td><td align="center" valign="middle" >m 2 − 2 2</td><td align="center" valign="middle" >1 4</td><td align="center" valign="middle" >ns ( ξ ) &#177; ds ( ξ )</td></tr><tr><td align="center" valign="middle" >14</td><td align="center" valign="middle" >m 2 4</td><td align="center" valign="middle" >m 2 − 2 2</td><td align="center" valign="middle" >m 2 4</td><td align="center" valign="middle" >sn ( ξ ) &#177; i   cn ( ξ )</td></tr></tbody></table></table-wrap><p>f ′ ( ξ ) = ϕ ( ξ ) = − 2 3 k ( m 2 + 1 ) + 2 k   ns 2 ( ξ , m ) , (41)</p><p>f ′ ( ξ ) = ϕ ( ξ ) = − 2 3 k ( m 2 + 1 ) + 2 k   dc 2 ( ξ , m ) . (42)</p><p>Therefore, solutions of Equation (1) can be expressed as</p><p>u ( x , y , z , t ) = f ( ξ ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) = − 2 3 k ( m 2 + 1 ) ξ − 2 k   EllipticE ( sn ( ξ , m ) , m )         − 2 k ds ( ξ , m ) cs ( ξ , m ) ns ( ξ , m ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) . (43)</p><p>u ( x , y , z , t ) = f ( ξ ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) = − 2 3 k ( m 2 + 1 ) ξ − 2 k   EllipticE ( sn ( ξ , m ) , m )     + 2 k dc ( ξ , m ) sc ( ξ , m ) nc ( ξ , m ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) . (44)</p><p>when m → 1 , ns ( ξ , m ) → c o t h ( ξ ) , solution (41) becomes</p><p>f ′ ( ξ ) = ϕ ( ξ ) = − 4 k 3 + 2 k coth 2 ( ξ ) . (45)</p><p>Thus, one has</p><p>u ( x , y , z , t ) = f ( ξ ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) = − 4 k 3 ξ − k ( 2 coth ( ξ ) − ln 1 + coth ( ξ ) 1 − coth ( ξ ) )     + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) . (46)</p><p>when m → 0 , ns ( ξ , m ) → c s c ( ξ ) , solution (41) becomes</p><p>f ′ ( ξ ) = ϕ ( ξ ) = − 4 k 3 + 2 k csc 2 ( ξ ) . (47)</p><p>Thus, one has</p><p>u ( x , y , z , t ) = f ( ξ ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) = − 4 k 3 ξ − 2 k cot ( ξ ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) . (48)</p><p>when m → 0 , dc ( ξ , m ) → s e c ( ξ ) , solution (42) becomes</p><p>f ′ ( ξ ) = ϕ ( ξ ) = − 4 k 3 + 2 k sec 2 ( ξ ) . (49)</p><p>Thus, one has</p><p>u ( x , y , z , t ) = f ( ξ ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) = − 4 k 3 ξ − 2 k tan ( ξ ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) . (50)</p><p>when m → 1 , dc ( ξ , m ) → 1 , solution (42) becomes</p><p>f ′ ( ξ ) = ϕ ( ξ ) = − 4 k 3 . (51)</p><p>Thus, one has</p><p>u ( x , y , z , t ) = f ( ξ ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) = − 4 k 3 ξ + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) . (52)</p><p>From (39), we have</p><p>f ′ ( ξ ) = ϕ ( ξ ) = − 2 3 k ( m 2 + 1 ) + 2 k m 2 sn 2 ( ξ , m ) , (53)</p><p>f ′ ( ξ ) = ϕ ( ξ ) = − 2 3 k ( m 2 + 1 ) + 2 k m 2 cd 2 ( ξ , m ) . (54)</p><p>Therefore, solutions of Equation (1) can be expressed as</p><p>u ( x , y , z , t ) = f ( ξ ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) = − 2 3 k ( m 2 − 2 ) ξ − 2 k   EllipticE ( sn ( ξ , m ) , m )     + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) . (55)</p><p>u ( x , y , z , t ) = f ( ξ ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) = − 2 3 k ( m 2 − 2 ) ξ − 2 k   EllipticE ( sn ( ξ , m ) , m )     + 2 k m 2 sd ( ξ , m ) cd ( ξ , m ) nd ( ξ , m ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) . (56)</p><p>when m → 1 , sn ( ξ , m ) → t a n h ( ξ ) , solution (53) becomes</p><p>f ′ ( ξ ) = ϕ ( ξ ) = − 4 k 3 + 2 k tanh 2 ( ξ ) , (57)</p><p>Thus, one has</p><p>u ( x , y , z , t ) = f ( ξ ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) = − 4 k 3 ξ − k ( 2 tanh ( ξ ) − ln 1 + tanh ( ξ ) 1 − tanh ( ξ ) )     + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) . (58)</p><p>From (40), we have</p><p>f ′ ( ξ ) = ϕ ( ξ ) = − 2 3 k ( m 2 + 1 ) + 2 k m 2 sn 2 ( ξ , m ) + 2 k   ns 2 ( ξ , m ) , (59)</p><p>f ′ ( ξ ) = ϕ ( ξ ) = − 2 3 k ( m 2 + 1 ) + 2 k m 2 cd 2 ( ξ , m ) + 2 k   dc 2 ( ξ , m ) . (60)</p><p>Therefore, solutions of Equation (1) can be expressed as</p><p>u ( x , y , z , t ) = f ( ξ ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) = − 2 3 k ( m 2 − 5 ) ξ − 4 k   EllipticE ( sn ( η , m ) , m )     − 2 k ds ( ξ , m ) cs ( ξ , m ) ns ( ξ , m ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) . (61)</p><p>u ( x , y , z , t ) = f ( ξ ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) = − 2 3 k ( m 2 − 5 ) ξ − 4 k   EllipticE ( sn ( η , m ) , m )     + 2 k dc ( ξ , m ) sc ( ξ , m ) nd ( ξ , m ) + 2 k m 2 sd ( ξ , m ) cd ( ξ , m ) nd ( ξ , m )     + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) . (62)</p><p>when m → 1 , sn ( ξ , m ) → t a n h ( ξ ) , solution (59) becomes</p><p>f ′ ( ξ ) = ϕ ( ξ ) = − 4 k 3 + 2 k tanh 2 ( ξ ) + 2 k coth 2 ( ξ ) , (63)</p><p>Thus, one has</p><p>u ( x , y , z , t ) = f ( ξ ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) = − 4 k 3 ξ − 2 k ( tanh ( ξ ) + coth ( ξ ) )     + k ln ( 1 + tanh ( ξ ) ) ( 1 + coth ( ξ ) ) ( 1 − tanh ( ξ ) ) ( 1 − cot ( ξ ) ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) . (64)</p><p>Remark 1. Let F ( ξ ) in (33) satisfies the following equation</p><p>( F ′ ( ξ ) ) 2 = h 0 + h 1 F ( ξ ) + h 3 F 3 ( ξ ) , (65)</p><p>where h 0 , h 1 and h 3 are constant. In this situation, we have the following result.</p><p>A 0 = 0 , A 1 = 1 2 k h 3 , A 2 = 0 , B 1 = 0 , B 2 = 0. (66)</p><p>Substituting Equation (66) into (33), we obtain the following solution of Equation (32):</p><p>ϕ ( ξ ) = 1 2 k h 3 F ( ξ ) . (67)</p><p>where ξ = k x + b Y + c z = k x + b ( y − ∫ F 3 ( t ) d t ) + c t .</p><p>The solution of Equation (65) is the Weierstrass elliptic doubly periodic type solution:</p><p>F ( ξ ) = WeierstrassP ( h 3 2 ξ , g 2 , g 3 ) , h 3 &gt; 0. (68)</p><p>where g 2 = − 4 h 1 h 3 , g 3 = − 4 h 0 h 3 and h 3 &gt; 0 . Substituting Equation (68) into (67), the solution of Equation (32) is</p><p>f ′ ( ξ ) = ϕ ( ξ ) = 1 2 k h 3   WeierstrassP ( h 3 2 ξ , g 2 , g 3 ) . (69)</p><p>Therefore, exact solutions of Equation (1) can be expressed</p><p>u ( x , y , z , t ) = f ( ξ ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) = −   k h 3   WeierstrassZeta ( h 3 2 ξ , g 2 , g 3 ) + ∫ F 2 ( z , t ) d t − x 4 F 3 ( t ) . (70)</p></sec><sec id="s4_2"><title>4.2. Solutions of Equation (19)</title><p>Using a traveling wave variable of Equation (19) as</p><p>U ( x , Y , Z ) = f ( ξ ) ,   ξ = k x + b Y + c Z . (71)</p><p>where Y = y − ∫ 1 F 4 ( z ) d z , Z = t − ∫ 1 F 4 ( z ) d z and k , b and c are constants, Equation (19) can be reduced to the following ODE</p><p>b   k 2 f ( 5 ) + c   f ‴ − 6 b k   f ′ f ‴ − 6 b k   f ″ 2 = 0 , (72)</p><p>where f ′ = d f d ξ , f ″ = d 2 f d ξ 2 , ⋯ . If let f ′ ( ξ ) = ϕ ( ξ ) , then (72) becomes</p><p>b   k 2 ϕ ( 4 ) + c ϕ ″ − 6 b k ϕ ϕ ″ − 6 b k ϕ ′ 2 = 0, (73)</p><p>Balancing ϕ ( 4 ) and ϕ ′ 2 in (73), we obtain n + 4 = 2 ( n + 1 ) which gives n = 2 . Suppose that Equation (73) owns the solutions in the form</p><p>ϕ ( ξ ) = A 0 + A 1 F ( ξ ) + A 2 F 2 ( ξ ) + B 1 F ( ξ ) + B 2 F ( ξ ) 2 , (74)</p><p>where F ( ξ ) satisfies the following equation</p><p>( F ′ ( ξ ) ) 2 = h 0 + h 2 F 2 ( ξ ) + h 4 F 4 ( ξ ) , (75)</p><p>where h 0 , h 2 and h 4 are constant.</p><p>Substituting (74) and (75) into Equation (73) and then setting all the coefficients of F k ( k = − 6 , ⋯ , 6 ) of the resulting system to zero, we can obtain the following results.</p><p>A 0 = 4   b k 2 h 2 + c 6 b k , A 1 = 0 , A 2 = 0 , B 1 = 0 , B 2 = 2   k h 0 , (76)</p><p>A 0 = 4   b k 2 h 2 + c 6 b k , A 1 = 0 , A 2 = 2   k h 4 , B 1 = 0 , B 2 = 0 , (77)</p><p>A 0 = 4   b k 2 h 2 + c 6 b k , A 1 = 0 , A 2 = 2   k h 4 , B 1 = 0 , B 2 = 2   k h 0 , (78)</p><p>where h 0 , h 2 and h 4 are arbitrary constants, k , b and c are nonzero constants.</p><p>Substituting (76)-(78) into (74), we obtain respectively the following solutions of Equation (73)</p><p>ϕ ( ξ ) = 4 b k 2 h 2 + c 6 b k + 2 k h 0 F ( ξ ) 2 , (79)</p><p>ϕ ( ξ ) = 4 b k 2 h 2 + c 6 b k + 2 k h 4 F ( ξ ) 2 , (80)</p><p>ϕ ( ξ ) = 4 b k 2 h 2 + c 6 b k + 2 k h 0 F 2 ( ξ ) + 2 k h 4 F ( ξ ) 2 , (81)</p><p>where ξ = k x + b y − ( b + c ) ∫ 1 F 4 ( z ) d z + c t .</p><p>Substituting F ( ξ ) in <xref ref-type="table" rid="table1">Table 1</xref>, we can got<inline-formula><inline-graphic xlink:href="/html.scirp.org/file/13-1722024x225.png" xlink:type="simple"/></inline-formula>. Then by solving <inline-formula><inline-graphic xlink:href="/html.scirp.org/file/13-1722024x226.png" xlink:type="simple"/></inline-formula> and using<inline-formula><inline-graphic xlink:href="/html.scirp.org/file/13-1722024x227.png" xlink:type="simple"/></inline-formula>, we can obtain solutions of Equation (1). The procedure is similar. We omit it for simplicity.</p></sec></sec><sec id="s5"><title>5. Figures of Some Exact Solutions</title><p>The obtained solutions include some arbitrary functions. Taking some special functions we can get different solutions and graphics. In order to better understand the solutions, some typical figures of the solutions are given as follows:</p><p>In <xref ref-type="fig" rid="fig1">Figure 1</xref>, <inline-formula><inline-graphic xlink:href="/html.scirp.org/file/13-1722024x228.png" xlink:type="simple"/></inline-formula>, which is a travelling wave transformation and the figure is a classic periodic wave.</p><p>In <xref ref-type="fig" rid="fig2">Figure 2</xref>, <inline-formula><inline-graphic xlink:href="/html.scirp.org/file/13-1722024x229.png" xlink:type="simple"/></inline-formula>, which is not a travelling wave transformation and the figure is a unknown one.</p><p>In <xref ref-type="fig" rid="fig3">Figure 3</xref>, <inline-formula><inline-graphic xlink:href="/html.scirp.org/file/13-1722024x230.png" xlink:type="simple"/></inline-formula>, which is not a travelling wave transformation and the figure is unknown.</p><p>In <xref ref-type="fig" rid="fig4">Figure 4</xref>, <inline-formula><inline-graphic xlink:href="/html.scirp.org/file/13-1722024x235.png" xlink:type="simple"/></inline-formula>, which is a travelling wave transformation and the figure is a plane.</p><p>In <xref ref-type="fig" rid="fig5">Figure 5</xref>, <inline-formula><inline-graphic xlink:href="/html.scirp.org/file/13-1722024x236.png" xlink:type="simple"/></inline-formula>, which is not a travelling wave transformation and the figure is a solitary wave.</p><p>In <xref ref-type="fig" rid="fig6">Figure 6</xref>, <inline-formula><inline-graphic xlink:href="/html.scirp.org/file/13-1722024x237.png" xlink:type="simple"/></inline-formula>, which</p><p>is not a travelling wave transformation and the figure is a kink wave.</p></sec><sec id="s6"><title>6. Conclusions</title><p>In this manuscript, a higher-dimensional shallow water wave Equation (1) is studied by Lie symmetry analysis method and extended F-expansion method and some new exact solutions are obtained. It is interesting that these solutions contain some arbitrary functions <inline-formula><inline-graphic xlink:href="//html.scirp.org/file/13-1722024x246.png" xlink:type="simple"/></inline-formula> and<inline-formula><inline-graphic xlink:href="//html.scirp.org/file/13-1722024x246.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="//html.scirp.org/file/13-1722024x247.png" xlink:type="simple"/></inline-formula>. Taking these functions as special ones, we can get nonlinear wave solutions and wave solutions of Equation (1). The method is effective to high-dimensional differential equations, and can also be applied to other nonlinear evolution ones. Our main work list as follows:</p><p>&#183; All of the geometric vector fields of the equation are obtained.</p><p>&#183; The symmetry reductions are presented.</p><p>&#183; Some new linear and nonlinear wave solutions are obtained.</p><p>&#183; Some typical figures are given.</p></sec><sec id="s7"><title>Acknowledgements</title><p>This research is supported by innovation and entrepreneurship training Program of university Students of Yunnan (DCXM193009) and innovation and entrepreneurship training Program of university Students of Honghe University (DCXL181045).</p></sec><sec id="s8"><title>Conflicts of Interest</title><p>The authors declare no conflicts of interest regarding the publication of this paper.</p></sec><sec id="s9"><title>Cite this paper</title><p>Dong, L.M., Guo, Z. and He, Y.H. (2020) Some New Nonlinear Wave Solutions for a Higher-Dimensional Shallow Water Wave Equation. Journal of Applied Mathematics and Physics, 8, 1845-1860. https://doi.org/10.4236/jamp.2020.89139</p></sec></body><back><ref-list><title>References</title><ref id="scirp.102941-ref1"><label>1</label><mixed-citation publication-type="other" xlink:type="simple">Liu, H.Z. and Li, J.B. (2014) Symmetry Reductions, Dynamical Behavior and Exact Explicit Solutions to the Gordon Types of Equations. Journal of Computational and Applied Mathematics, 257, 144-56. https://doi.org/10.1016/j.cam.2013.08.022</mixed-citation></ref><ref id="scirp.102941-ref2"><label>2</label><mixed-citation publication-type="other" xlink:type="simple">Liu, H.Z. and Geng, Y.X. (2013) Symmetry Reductions and Exact Solutions to the Systems of Carbon Nanotubes Conveying Fluid. Journal of Differential Equations, 254, 2289-2303. https://doi.org/10.1016/j.jde.2012.12.004</mixed-citation></ref><ref id="scirp.102941-ref3"><label>3</label><mixed-citation publication-type="other" xlink:type="simple">Fan, E. (2003) Uniformly Constructing a Series of Explicit Exact Solutions to Nonlinear Equations in Mathematical Physics. Chaos, Solitons and Fractals, 16, 819-839. https://doi.org/10.1016/S0960-0779(02)00472-1</mixed-citation></ref><ref id="scirp.102941-ref4"><label>4</label><mixed-citation publication-type="other" xlink:type="simple">Yomba, E. (2005) The Extended Fan’s Sub-Equation Method and Its Application to KdV-MKdV, BKK and Variant Boussinesq Equations. Physics Letters A, 336, 463-476. https://doi.org/10.1016/j.physleta.2005.01.027</mixed-citation></ref><ref id="scirp.102941-ref5"><label>5</label><mixed-citation publication-type="other" xlink:type="simple">Wazwaz, A.M. (2009) Multiple-Soliton Solutions and Multiple-Singular Soliton Solutions for Two Higher-Dimensional Shallow Water Wave Equations. Applied Mathematics and Computation, 211, 495-501. https://doi.org/10.1016/j.amc.2009.01.071</mixed-citation></ref><ref id="scirp.102941-ref6"><label>6</label><mixed-citation publication-type="other" xlink:type="simple">Clarkson, P.A., Mansfield, E.L. and Mansfield, E.L. (1994) On a shallow Water Wave Equation. Nonlinearity, 7, 975-1000. https://doi.org/10.1088/0951-7715/7/3/012</mixed-citation></ref><ref id="scirp.102941-ref7"><label>7</label><mixed-citation publication-type="other" xlink:type="simple">Chen, Y.R. and Liu, R. (2015) Some New Nonlinear Wave Solutions for Two (3+1)-Dimensional Equations. Applied Mathematics and Computation, 260, 397-411. https://doi.org/10.1016/j.amc.2015.03.098</mixed-citation></ref><ref id="scirp.102941-ref8"><label>8</label><mixed-citation publication-type="other" xlink:type="simple">Hirota, R. (2004) The Direct Method in Soliton Theory. Cambridge University Press, Cambridge. https://doi.org/10.1017/CBO9780511543043</mixed-citation></ref><ref id="scirp.102941-ref9"><label>9</label><mixed-citation publication-type="other" xlink:type="simple">Hirota, R. (1971) Exact Solutions of the Korteweg-Devries Equation for Multiple Collisions of Solutions. Physical Review Letters, 27, 1192-1194. https://doi.org/10.1103/PhysRevLett.27.1192</mixed-citation></ref><ref id="scirp.102941-ref10"><label>10</label><mixed-citation publication-type="other" xlink:type="simple">Li, J.B. and Liu, Z.R. (2000) Smooth and Non-Smooth Traveling Waves in a Nonlinearly Dispersive Equation. Applied Mathematical Modelling, 25, 41-56. https://doi.org/10.1016/S0307-904X(00)00031-7</mixed-citation></ref></ref-list></back></article>