a reduced model for internal waves interacting with submarine ...
a reduced model for internal waves interacting with submarine ...
a reduced model for internal waves interacting with submarine ...
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i. e. u 1z =βw 1x . Hence ( )<br />
u (0)<br />
1<br />
= 0 and as expected <strong>for</strong> shallow water flows u(0)<br />
z 1<br />
is<br />
independent from z:<br />
u (0)<br />
1<br />
= u (0) (x, t). (2.12)<br />
1<br />
We now correct this first order approximation. By using<br />
u 1 = u (0)<br />
1<br />
+βu (1)<br />
1<br />
+ O(β 2 ) (2.13)<br />
and Eq. (2.12) it is straight<strong>for</strong>ward that<br />
∫ 1<br />
η<br />
∫1<br />
u 2 1 dz=<br />
u 2 1 = u(0)<br />
2<br />
1 + 2βu<br />
(1)<br />
1 u(0) 1<br />
+ O(β 2 ),<br />
η<br />
u (0)<br />
1<br />
∫1<br />
2<br />
dz+2β<br />
η<br />
u (1)<br />
1 u(0) 1<br />
dz+O(β 2 ),<br />
and<br />
η 1 u 1· u 1 = u (0) 2<br />
1 (1−η)+2η1 βu (0)<br />
1 u(1) 1<br />
+ O(β 2 ),<br />
so that<br />
Also from Eq. (2.13),<br />
u 1· u 1 = u (0)<br />
1<br />
· u (0)<br />
1<br />
+ 2βu (0)<br />
1 u(1) 1<br />
+ O(β 2 ). (2.14)<br />
∫1<br />
1<br />
u 1 dz=u (0)<br />
1<br />
+βu (1)<br />
1<br />
+ O(β 2 ),<br />
η 1<br />
η<br />
u 1 = u (0)<br />
1<br />
+βu (1)<br />
1<br />
+ O(β 2 ),<br />
u 1· u 1 = u (0)<br />
1<br />
· u (0)<br />
1<br />
+ 2βu (0)<br />
1 u(1) 1<br />
+ O(β 2 ). (2.15)<br />
16