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\chapter{結論}
本論文では, 惑星大気大循環モデル DCPAM5 を用いて計算したモデル地球が, 現実地球の気候をどの程度表現することができるかを調べた. モデル地球と現実地球の気候の比較を行う際には, 気温と降水量の二つの変数から気候区分を決定できるケッペンの気候区分を用いた. T21L26, T42L26 の二種類の解像度で実験を行った結果, T21L26 解像度では, 気候区分は現実地球と概ね同じ領域に表現された. しかし, 中国北部やアラビア半島南部, グリーンランド中部の気候区分が現実地球と異なり, これは地形や風, アルベドの値の違いから生じていると考えられる. T42L26 解像度でも, 気候区分は現実地球と概ね同じ領域に表現された. 上で挙げたグリーンランド中部に関しては, T21L26 解像度とは違い, 現実地球と同じ気候区分に表現された. しかし, 中国北部, アラビア半島南部に関しては, T21L26 解像度と同様, 現実地球と異なる気候区分に表現された.

まとめると, どちらの解像度の実験でも, アルベドや地形の違いから現実地球と異なる気候区分に表現された領域もあったが, 気候区分は概ね現実地球と同じ領域に表現された. つまり, 現実地球のパラメータ等を設定すると, DCPAM5 は現実地球と類似した気候を計算できることがわかった. 

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