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% Dennou-SOGCM
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%   2015/06/15  海洋モデル 定式化
%               河合　佑太
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\Dauthor{河合佑太}        % 担当者の名前
\Ddate{2015/06/16}        % 変更日時 (毎回変更すること)
\Dfile{formulatiom.tex}

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\begin{document}

\chapter{海氷熱力学モデルの定式化}

\section{系の設定}
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\begin{figure}[b]]
 \includegraphics[width=10cm]{seaice_therm_model_config.eps}
 \caption{系の設定}
 \label{fig:configuration}
\end{figure} 
%%
多くの海氷熱力学モデル\citep{maykut1971some,semtner1976model,winton2000reformulated}は,
海氷を図\ref{fig:configuration}のような雪層と氷層から成る鉛直一次元のカラムとして考える. 
また, 海氷の上端では大気, 下端では海洋に接しており, 
そこで海氷は大気や海洋と熱のやりとりをする.

雪層や氷層内の鉛直温度分布は, 各層において熱伝導方程式を解くによって決定される.
この熱伝導方程式に課す境界条件は, 大気からの熱フラックスや海洋から熱フラックス
である. 
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\include{./governeq}
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\include{./seaice_specheat}

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\end{document}