lsd-zf/main.tex
2023-02-02 18:13:28 +01:00

187 lines
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TeX

\documentclass[8pt,landscape]{article}
\usepackage{multicol}
\usepackage{calc}
\usepackage{bookmark}
\usepackage{ifthen}
\usepackage[a4paper, landscape]{geometry}
\usepackage{hyperref}
\usepackage{ccicons}
\usepackage{amsmath, amsfonts, amssymb, amsthm}
\usepackage{listings}
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\usepackage{float}
\usepackage{apacite}
\usepackage[
type={CC},
modifier={by-sa},
version={3.0}
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% To make this come out properly in landscape mode, do one of the following
% 1.
% pdflatex latexsheet.tex
%
% 2.
% latex latexsheet.tex
% dvips -P pdf -t landscape latexsheet.dvi
% ps2pdf latexsheet.ps
% If you're reading this, be prepared for confusion. Making this was
% a learning experience for me, and it shows. Much of the placement
% was hacked in; if you make it better, let me know...
% 2008-04
% Changed page margin code to use the geometry package. Also added code for
% conditional page margins, depending on paper size. Thanks to Uwe Ziegenhagen
% for the suggestions.
% 2006-08
% Made changes based on suggestions from Gene Cooperman. <gene at ccs.neu.edu>
% To Do:
% \listoffigures \listoftables
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% This sets page margins to .5 inch if using letter paper, and to 1cm
% if using A4 paper. (This probably isn't strictly necessary.)
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% Turn off header and footer
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% Don't print section numbers
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% -----------------------------------------------------------------------
\begin{document}
\raggedright
\footnotesize
\begin{multicols*}{3}
% multicol parameters
% These lengths are set only within the two main columns
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\begin{center}
\Large{Dynamics of Large-scale Atmospheric Flow} \\
\small{\href{http://iacweb.ethz.ch/courses/id/701-1221-00L}{701-1221-00}} \\
\small{Jannis Portmann \the\year} \\
{\ccbysa}
\rule{\linewidth}{0.25pt}
\end{center}
\section{Equations}
\subsection{Navier-Stokes}
\begin{equation}
\frac{D}{Dt}
\end{equation}
\subsection{Circulation}
\begin{equation}
C = \oint_c u \, dc = \oint (u \, dx + v \, dy + w \, dz)
\end{equation}
\section{Concepts}
\subsection{Thermal wind}
\textit{Thermal wind} describes the vertical change of geostrophic (i.e. horizontal) wind
\begin{equation}
\frac{\partial}{\partial z} v_G = \bigg(\frac{1}{f}\frac{g}{\theta_0}\bigg)(k \times \nabla_h \theta^*)
\end{equation}
\scriptsize
\section*{Copyleft}
\doclicenseImage \\
This document is released under (CC BY-SA 3.0) \\
\faGlobeEurope \kern 1em \url{https://n.ethz.ch/~jannisp/lsd-zf} \\
\faGit \kern 0.88em \url{https://git.thisfro.ch/thisfro/lsd-zf} \\
Jannis Portmann, HS22
\section*{References}
\begin{enumerate}
\item Script: LSD\_22.pdf
\end{enumerate}
\section*{Image sources}
\begin{itemize}
\item Bild
\end{itemize}
\end{multicols*}
\end{document}