commit 15ad16c5a256b66892ea3ea60afe002b097a492e
parent 043c7e17fe45b0306c2e08053ee7334910ac9030
Author: Ivan Gankevich <igankevich@ya.ru>
Date: Thu, 18 Jul 2019 21:54:10 +0300
Translate introduction.
Diffstat:
2 files changed, 30 insertions(+), 0 deletions(-)
diff --git a/.gitignore b/.gitignore
@@ -304,4 +304,14 @@ tags
# End of https://www.gitignore.io/api/vim,latex,linux
+# Created by https://www.gitignore.io/api/libreoffice
+# Edit at https://www.gitignore.io/?templates=libreoffice
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+# LibreOffice locks
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+# End of https://www.gitignore.io/api/libreoffice
+
+
build
diff --git a/main.tex b/main.tex
@@ -57,6 +57,26 @@ that uses added masses.
\section{Introduction}
+Ship and sea wavy surface motion do not have an abundance of geometric forms
+and physical phenomena. Waves formation due to ship motion and interaction
+between ocean and atmosphere are governed by continuity condition for heavy
+fluid and the law of conservation of energy: wind waves have uniform energy
+distribution.
+
+Strict theoretical solution (and in fact the only solution) for large-amplitude
+wind waves on the surface of heavy fluid was obtained in 1802 by Franz Josef
+von Gerstner~--- a professor from a university in Prague~\cite{gerstner1809}.
+Generic trochoidal wave mathematical model has high
+dispersion~\cite{sommerfeld1945mechanik}, the dependence of the speed of wave
+crest propagation on their length and period. As a result
+\begin{itemize}
+ \item wave energy propagation speed becomes half the visible phase velocity
+ of wave crests,
+ \item wave front constantly changes its phase, and
+ \item wave are quantised into packets and wave transformation
+ and propagation phenomena become nonstationary.
+\end{itemize}
+
\section{Computational model of intense sea waves}
\begin{figure}