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Appendix B<br />

The Dirichlet-to-Neumann operator<br />

Due to the importance of the Dirichlet-to-Neumann operator (DtN 0 ) in <strong>model</strong>ling<br />

water <strong>waves</strong> we pointed here its relation <strong>with</strong> the Hilbert trans<strong>for</strong>m on the flat strip<br />

used througout this work.<br />

Given the problem<br />

⎧<br />

⎪⎨<br />

⎪⎩<br />

z υυ + z ωω = 0, −h≤ω≤0,<br />

z ω = g(υ), ω=0,<br />

z ω = 0, ω=−h,<br />

the operatorT returns the tangential derivative z υ (υ, 0) from the Neumann data<br />

z ω (υ, 0)=g(υ), that is<br />

T [g]=z υ (υ, 0).<br />

There<strong>for</strong>e, its inverseT satisfies<br />

g(υ)=z ω (υ, 0)=T [z υ (υ, 0)].<br />

(B.1)<br />

91

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