上部海洋の温暖化と数十年にわたる海面上昇の改善された推定値
Catia M Domingues1, John A Church, Neil J White
1Centre for Australian Weather and Climate Research, CSIRO Marine and Atmospheric Research, GPO Box 1538, Hobart, Tasmania 7001, Australia. catia.domingues@csiro.au
Nature
|June 20, 2008
まとめ
海洋の熱含量と熱膨張は,海面上昇に大きく寄与しています. 改善された海洋温度のデータは,より高い温暖化傾向を明らかにし,気候モデルを観測された海面上昇とより良く整合させていますが,数十年にわたる傾向は依然として異なります.
科学分野:
- 気候科学 気候科学
- 海洋学 海洋学とは
- 海面上昇 海面上昇
背景:
- 海洋温度と熱膨張は,気候システムのエネルギー予算と海面上昇の重要な指標である.
- 気候モデルは,稀なデータとモデルの限界のために,地球規模の海洋熱含有量における観察された10年間の変動を複製するために苦労します.
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