Application of Homotopy and Variational Iteration Methods to the Atmospheric Internal Waves Model

ISSN: 2319-765X

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Journal of
Mathematics
Volume 10. Issue 5. Version 5
September-October 2014

IOSR Journals
International Or9Jn1zat1on
of Sc1ent1f1c Reso.:arc!'!

IOSR Journal of Mathematics (IOSR-JM) is a douhll' blind pl'

(16)


The right hand sidt! of equation ( 1-t) depends onl) on the 1crrn"> li:u-: Thu'-. \\I..' t'a") h) nbtain th1..•
series of Um,nl = 1,2,3, ... by solving the linear high-order defonnation equation ) オセゥョァ@
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computation sofhvare such as Maple. tv1atlab or \l1L·ric /ntt'rnal

vm (x. t) ;;;; Xm vm-1 (x, t)

f'
f'

+ h2 'R.2.m (um-I• vm-1 •hm-1) ds
0

hm(x,t) = Xmh 111 _ 1(x.t) + h:i

.'.R:i.: 11 (Um-J•V:u-i•hm-l)ds

u

Where,


セ@

AJ,m

(-

-

Um-1• Vm-1•

-h

m-1

)

m-1
"\'


aum-1

="at+ L

aum-i-..

ax

Un

n=O

I
=-,-+
i
I
+

m-1


.....
'R.2m(um-t•Ym-1•hm-1)
·

avm-1

- _ .'.R3.m (Um-I• Ym-1• hm-1

ahm-1

vt

avm-1

un-a-+fu 0
X

am-1

+gH,

vqm- 1

(27)

;::i-

n=O

m-1

= -iJt

ahm-1-n
iJ

Lin

n=O

x


+ hn

。オュMQセL@

J

c.x

+ V:11-1 II.

According to equation ( 12), the results of system (I) can be obtained by sol\'ing the following series:
+oo

L
+L
L

u(x, t) = u 0 (x, t) +


Um (x, t),

m=I
+oo

v(x. t) = v 0 (x, t)

v,,, (x, t),

t28)

m= I

h(x, t) = h 0 (x, t) +

hm(x, t).

m=I

4.2 Aplication of Variational Iteration Method

,
In this section, we implement VIM for obtaining the analytical approximate solution of system (I}. By
means of the variational iteration method refers to system (I), we construct correction functionals as follow

J'

uk+l (x, t) = u, +

'-1 co ( (u,J( + ii,(ii,), -

rv, + gii,(ii,)J 、セN@

0

t

Vk+I (x, t)

= v, + JAz(O( (v,)( +ii, (v,), + ru, + gH) d