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東亞冬季季風:年代際變化、突變與減弱趨勢

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圖 1.1:1948 年至 2012 年 NCEP Re-analysis 冬季氣候平均場,a 為海平面氣 壓場,b 為 850 hPa 風場。
圖 1.2:同圖 1.1,但 c 為 500 hPa 重力位高度場,d 為 200 hPa 緯向風場。
圖 2.1:上圖為 PDO 指數與全球海表面溫度的迴歸係數(陸地上則為地表溫度,
圖 2.2:AO 處於正相位(左圖)與負相位(右圖)時,北美洲與歐洲受影響之 示意圖。此圖來自 http://www.nasa.gov/。
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