Internal Wave Generation in Uniformly Stratified Fluids. 1 ... - LEGI
Internal Wave Generation in Uniformly Stratified Fluids. 1 ... - LEGI
Internal Wave Generation in Uniformly Stratified Fluids. 1 ... - LEGI
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
educes to the Green’s function. Now, if the <strong>in</strong>itial state of the fluid is taken just before the<br />
impulse, at t = 0 – , ψ 0 (r) = 0, ψ 1 (r) = 0, m(r, t) = δ(r) δ(t) and G(r, t) arises from the mass source<br />
term <strong>in</strong> (B3). If, on the other hand, the <strong>in</strong>itial state refers to t = 0 + , just after the impulse,<br />
irrotational <strong>in</strong>itial conditions are ψ 0 (r) = 0 and ψ 1 (r) = – 1/(4πr), while m(r, t) = 0; G(r, t) arises<br />
now from the <strong>in</strong>itial data term <strong>in</strong> (B3), by virtue of Δ (1/r) = – 4π δ(r). Thus, the equivalence of<br />
both approaches is proved for the Green’s function. As any <strong>in</strong>ternal wave field may be built<br />
by a superposition of elementary impulses, this conclusion is at the same time proved from a<br />
general po<strong>in</strong>t of view.<br />
<strong>Internal</strong> wave generation. 1. Green’s function 49