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最後の氷河期間の世界の海洋温度の平均値
Bernhard Bereiter1,2,3, Sarah Shackleton1, Daniel Baggenstos1,2
1Scripps Institution of Oceanography, University of California San Diego, La Jolla, California 92037, USA.
Nature
|January 5, 2018
まとめ
海の温度は 氷河期に大きく上昇しました この研究では 氷の核にある高貴なガスを用いて 海洋温度の変化を 1万年にわたって再構築しました
科学分野:
- 古代気候学
- 海洋学
- 気候科学
背景:
- 気候変動に対する長期の海洋温度の反応に関するデータは限られている.
- 海洋が長期間にわたって 人為的な熱を吸収する役割は不明である.
研究 の 目的:
- 高精度で時間的な解像度で 過去の海洋温度を再現します
- 海洋温度と南極の温度と 大気中のCO2レベルとの関係を調べるため
- 地球の気候の歴史における 急激な温暖化現象を分析するためです
主な方法:
- 氷の核に保存された高貴なガスを利用し,古気候を再構築した.
- 総合的な世界の海洋温度を推定するための新しい方法を開発しました.
- 南極の気温と大気中のCO2記録と相関する海洋温度データ
主要な成果:
- 地球の海洋温度は2万~1万年前から2.57±0.24°C上昇した.
- 大気中のCO2に対してリードや遅滞がない.
- 近代的な海洋熱吸収の見積もりを上回る 700年間の温暖化現象を特定した.
結論:
- 南半球の気候は,世界の気候傾向に大きな影響を与える.
- 氷の核における高貴なガスの分析は,世界の海洋温度の再構築のための堅固な方法を提供します.
- 過去の急激な海洋温暖化は 気候変動の感受性に関する 洞察力を与えてきました
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