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\chapter{はじめに}

テレコネクションとは, 地球上の遠く離れた場所における温度や圧力などの気象学的なパラメータが, 互いに相関をもって変動する現象である.  
また, いくつかの空間分布がテレコネクションによって生じていることが知られている. 
本論文ではテレコネクションパターンのひとつである, 北半球冬季の対流圏中層に現れる太平洋・北米パターンの特徴を示す. 
これは対流圏中層において, カナダ西岸に沿ってブロッキングが起こる空間分布と, 西から東へと等高度線が一直線な空間分布を引き起こす. 
本論文では, この太平洋・北米パターンについて, Wallace and Gutzler (1981) で説明された 500 hPa ジオポテンシャル高度, 海面更生気圧, 1000 - 500 hPa 層厚に加えて, 地表面温度の特徴を説明する. \\
\vspace{12pt} \\
　本論文の構成は以下の通りである. 
2 章では, 使用したデータや解析手法を説明する. 
3 章では, 解析により得られた 500 hPa ジオポテンシャル高度, 海面更生気圧, 1000 - 500 hPa 層厚, 地表面温度の特徴を説明する. 
4 章では, 3 章で説明した特徴が定常ロスビー波の現れであることを示す. 
5 章で結論を述べる. 






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