海洋学. 海洋学. 北太平洋のアノキシアの百年にわたる変化は,熱帯の貿易風に関連しています
Curtis Deutsch1, William Berelson2, Robert Thunell3
1School of Oceanography, University of Washington, Seattle, WA, USA. cdeutsch@uw.edu.
まとめ
海洋温暖化は,世界の脱酸素化傾向にもかかわらず,風が変化しているため,北太平洋の酸素最小限区域 (OMZ) が縮小しています. これは,海洋酸素レベルが低下するにつれて,OMZの範囲が収縮する可能性があることを示唆しています.
科学分野:
- 海洋学 海洋学 海洋学
- 気候科学 気候科学
- 地質化学 地質化学
背景:
- 気候の温暖化は,海洋の酸素 (O2) 供給を減少させ,酸素最小限ゾーン (OMZ) を拡大させる.
- 過去のOMZの動態を理解することは,将来の海洋脱酸素化の予測に不可欠です.
研究 の 目的:
- 1850年以降の北太平洋の無酸素の範囲を再構築する.
- OMZの変動と気候の要因との関係を調査する.
主な方法:
- デニトリフィケーション (δ(15) N) のために地化学的代理物を利用しました.
- 北太平洋の複数の堆積物核を分析した.
主要な成果:
- 1990年~以降のδ(15) Nの増加は,オキシオンの膨張を示し,O2の動向と一致しています.
- 前回の減少傾向は,20世紀の大部分にわたってOMZの収縮を示唆している.
- この2つの傾向は,熱帯太平洋の風の変化と相関しており,上流とO2需要に影響を及ぼしている.
結論:
- 太平洋の熱帯風は北太平洋のOMZの範囲に大きな影響を与えます.
- 将来の赤道太平洋風の弱まりは,OMZの収縮につながり,世界的な脱酸素化に対抗する可能性があります.
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